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EM-618: Potential outcomes of multi-variable climate change on water resources in the Santa Basin, Peru
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EM-618 | |
Document Author
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Van Soesbergen, A. and M. Mulligan |
Document Year
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2018 |
Change in ET ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in ET percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
ET seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Melt runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt water seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Rainfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snow pack seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snowfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Total runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Water balance seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
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Variable ID
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14660 | 14661 | 14662 | 14663 | 14666 | 14667 | 14664 | 14665 | 14656 | 14657 | 14658 | 14659 | 14670 | 14683 | 14678 | 14685 | 14672 | 14669 | 14673 | 14671 | 14681 | 14674 | 14684 | 14668 |
Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Melt Q | Melt Q | Melt Q | Not reported | Not reported | Not reported | Not reported | Total Q | Total Q | Total Q | Not reported | |
Qualitative-Quantitative
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Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) | Quantitative (Cardinal Only) |
Cardinal-Ordinal
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Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal | Cardinal |
mm yr^-1 | % | mm yr^-1 | % | mm yr^-1 | % | mm yr^-1 | % | mm yr^-1 | % | mm yr^-1 | % | unitless | m^3 s^-1 | m^3 s^-1 | m^3 s^-1 | unitless | unitless | unitless | unitless | m^3 s^-1 | m^3 s^-1 | m^3 s^-1 | unitless |
Change in ET ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in ET percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
ET seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Melt runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt water seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Rainfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snow pack seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snowfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Total runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Water balance seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
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Predictor-Intermediate-Response
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Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Response |
Predictor Variable Type
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Response Variable Type
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Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Computed Variable |
Data Source/Type
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Variable Classification Hierarchy
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5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
5. Ecosystem Attributes and Potential Supply of Ecosystem Goods and Services |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--CICES categories: Ecosystem goods and services - or landscape-level indices of suitability to supply EGS |
--CICES categories: Ecosystem goods and services - or landscape-level indices of suitability to supply EGS |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--Physical/chemical characteristics of nonliving ecosystem components |
--CICES categories: Ecosystem goods and services - or landscape-level indices of suitability to supply EGS |
--CICES categories: Ecosystem goods and services - or landscape-level indices of suitability to supply EGS |
--CICES categories: Ecosystem goods and services - or landscape-level indices of suitability to supply EGS |
--CICES categories: Ecosystem goods and services - or landscape-level indices of suitability to supply EGS |
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----Physical/chemical characteristics of water |
----Physical/chemical characteristics of water |
----Physical/chemical characteristics of air, meteorology and precipitation |
----Physical/chemical characteristics of air, meteorology and precipitation |
----Physical/chemical characteristics of air, meteorology and precipitation |
----Physical/chemical characteristics of air, meteorology and precipitation |
----Physical/chemical characteristics of water |
----Physical/chemical characteristics of water |
----Suitability to supply regulation & maintenance services-Mediation of flows |
----Suitability to supply regulation & maintenance services-Mediation of flows |
----Physical/chemical characteristics of air, meteorology and precipitation |
----Physical/chemical characteristics of air, meteorology and precipitation |
----Physical/chemical characteristics of water |
----Physical/chemical characteristics of water |
----Physical/chemical characteristics of water |
----Physical/chemical characteristics of water |
----Physical/chemical characteristics of water |
----Physical/chemical characteristics of air, meteorology and precipitation |
----Physical/chemical characteristics of water |
----Physical/chemical characteristics of air, meteorology and precipitation |
----Suitability to supply regulation & maintenance services-Mediation of flows |
----Suitability to supply regulation & maintenance services-Mediation of flows |
----Suitability to supply regulation & maintenance services-Mediation of flows |
----Suitability to supply regulation & maintenance services-Mediation of flows |
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------Evapotranspiration (via soil and/or vegetation) |
------Evapotranspiration (via soil and/or vegetation) |
------Meteorology data and parameters (including precipitation) |
------Meteorology data and parameters (including precipitation) |
------Meteorology data and parameters (including precipitation) |
------Meteorology data and parameters (including precipitation) |
------Other, multiple, unspecified or unclear |
------Other, multiple, unspecified or unclear |
------Hydrological cycle and water flow maintenance |
------Hydrological cycle and water flow maintenance |
------Meteorology data and parameters (including precipitation) |
------Meteorology data and parameters (including precipitation) |
------Evapotranspiration (via soil and/or vegetation) |
------Water volume or flow over ground surface (i.e., runoff) |
------Water volume or flow over ground surface (i.e., runoff) |
------Water volume or flow over ground surface (i.e., runoff) |
------Other, multiple, unspecified or unclear |
------Meteorology data and parameters (including precipitation) |
------Other, multiple, unspecified or unclear |
------Meteorology data and parameters (including precipitation) |
------Hydrological cycle and water flow maintenance |
------Hydrological cycle and water flow maintenance |
------Hydrological cycle and water flow maintenance |
------Hydrological cycle and water flow maintenance |
Change in ET ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in ET percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
ET seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Melt runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt water seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Rainfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snow pack seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snowfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Total runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Water balance seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
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Spatial Extent Area
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10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 | 10,000-100,000 km^2 |
Spatially Distributed?
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No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No |
Observations Spatially Patterned?
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Spatial Grain Type
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Spatial Grain Size
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Spatial Density
variable.detail.spDensityHelp
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
EnviroAtlas URL
variable.detail.enviroAtlasURLHelp
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Change in ET ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in ET percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
ET seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Melt runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt water seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Rainfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snow pack seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snowfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Total runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Water balance seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
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Temporal Extent
variable.detail.tempExtentHelp
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1950-2071 | 1950-2071 | 1950-2071 | 1950-2071 | 1950-2071 | 1950-2071 | 1950-2071 | 1950-2071 | 1950-2071 | 1950-2071 | 1950-2071 | 1950-2071 | 2071 | 2071 | 2071 | 2071 | 2071 | 2071 | 2071 | 2071 | 2071 | 2071 | 2071 | 2071 |
Temporally Distributed?
variable.detail.tempDistributedHelp
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No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No |
Regular Temporal Grain?
variable.detail.regularTempGrainHelp
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Temporal Grain Size Value
variable.detail.tempGrainSizeValHelp
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Temporal Grain Size Units
variable.detail.tempGrainSizeUnitHelp
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Temporal Density
variable.detail.tempDensityHelp
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Change in ET ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in ET percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
ET seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Melt runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt water seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Rainfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snow pack seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snowfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Total runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Water balance seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
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Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | |
Min Value
variable.detail.minEstHelp
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Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported |
Max Value
variable.detail.estHelp
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Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported | Not reported |
Other Value Type
variable.detail.natureOtherEstHelp
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Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value | Single Observation or Parameter Value |
Other Value
variable.detail.otherEstHelp
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Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values | Values vary by run; view runs to see values |
Change in ET ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in ET percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in fog inputs percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in snowmelt percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in water balance percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
Change in wind driven rainfall percent ?Comment:Modeled results for this response are presented as change relative to the simulated hydrological baseline for the period 1950-2000. |
ET seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Melt runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Melt water seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Rainfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snow pack seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Snowfall seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
Total runoff (Caraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Huaraz) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Total runoff (Santa outflow) ?Comment:Melt water contribution, total stream flow and melt water generated stream flow were analysed at the basin level (Santa outflow) and for two of the largest, most populous, high altitude cities in the basin: Caraz, with a population of circa 13,000 and Huaraz with a population of circa 96,000. |
Water balance seasonality ?Comment:To assess shifts in seasonality for the Rio Santa basin for all water balance fluxes, the seasonality index of Walsh and Lawler (1981) modified to handle negative values (by offsetting by the minimum so that all negatives become positive) was calculated using WaterWorld for the baseline and for the climate change scenarios for comparison. An index value of greater than 0.4 is considered seasonal, >0.8 marked seasonal with a long dry season and >1.2 extreme seasonal with almost all water available in 1-2 months. |
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Variability Expression Given?
variable.detail.variabilityExpHelp
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No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No |
Variability Metric
variable.detail.variabilityMetricHelp
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None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None |
Variability Value
variable.detail.variabilityValueHelp
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None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None |
Variability Units
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None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None |
Resampling Used?
variable.detail.bootstrappingHelp
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Variability Expression Used in Modeling?
variable.detail.variabilityUsedHelp
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Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Change in ET | Change in ET percent | Change in fog inputs | Change in fog inputs percent | Change in snowfall | Change in snowfall percent | Change in snowmelt | Change in snowmelt percent | Change in water balance | Change in water balance percent | Change in wind driven rainfall | Change in wind driven rainfall percent | ET seasonality | Melt runoff (Caraz) | Melt runoff (Huaraz) | Melt runoff (Santa outflow) | Melt water seasonality | Rainfall seasonality | Snow pack seasonality | Snowfall seasonality | Total runoff (Caraz) | Total runoff (Huaraz) | Total runoff (Santa outflow) | Water balance seasonality | |||||||||||||||||||||||||
Variable ID
variable.detail.varIdHelp
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14660 | 14661 | 14662 | 14663 | 14666 | 14667 | 14664 | 14665 | 14656 | 14657 | 14658 | 14659 | 14670 | 14683 | 14678 | 14685 | 14672 | 14669 | 14673 | 14671 | 14681 | 14674 | 14684 | 14668 | ||||||||||||||||||||||||
Validated?
variable.detail.resValidatedHelp
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No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | No | Yes | Yes | Yes | No | ||||||||||||||||||||||||
Validation Approach (within, between, etc.)
variable.detail.validationApproachHelp
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None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None |
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None | ||||||||||||||||||||||||
Validation Quality (Qual/Quant)
variable.detail.validationQualityHelp
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None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None |
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None | ||||||||||||||||||||||||
Validation Method (Stat/Deviance)
variable.detail.validationMethodHelp
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None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None |
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Validation Metric
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None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None |
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None | ||||||||||||||||||||||||
Validation Value
variable.detail.validationValHelp
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None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None |
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Validation Units
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None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None |
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Use of Measured Response Data
variable.detail.measuredResponseDataHelp
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None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None | None |