Watershed-Scale, Probabilistic Risk Assessment of Water Resources Impacts from Climate Change

A framework for the assessment of relative risk to watershed-scale water resources from systemic changes is presented. It is composed of two experiments, or pathways, within a Monte Carlo structure and provides quantification of prediction uncertainty. One simulation pathway is the no change, or nul...

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Main Author: Nick Martin
Format: Article
Language:English
Published: MDPI AG 2021-12-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/1/40
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spelling doaj-f7594abe1fb74e298853e2ac07a444292020-12-29T00:03:33ZengMDPI AGWater2073-44412021-12-0113404010.3390/w13010040Watershed-Scale, Probabilistic Risk Assessment of Water Resources Impacts from Climate ChangeNick Martin0Southwest Research Institute, San Antonio, TX 78253, USAA framework for the assessment of relative risk to watershed-scale water resources from systemic changes is presented. It is composed of two experiments, or pathways, within a Monte Carlo structure and provides quantification of prediction uncertainty. One simulation pathway is the no change, or null hypothesis, experiment, and the other provides simulation of the hypothesized system change. Each pathway uses a stochastic weather generator and a deterministic water balance model. For climate change impact analysis, the framework is calibrated so that the differences between thirty-year average precipitation and temperature pathway values reproduce climate trends. Simulated weather provides forcing for identical water balance models. Probabilistic time histories of differences in actual evapotranspiration, runoff, and recharge provide likelihood per magnitude change to water resources availability. The framework is applied to a semi-arid watershed in Texas. Projected climate trends for the site are a 3 °C increase in average temperature and corresponding increase in potential evapotranspiration, no significant change in average annual precipitation, and a semi-arid classification from 2011–2100. Two types of water balance model are used in separate applications: (1) monthly water balance and (2) daily distributed parameter. Both implementations predict no significant change, on average, to actual evapotranspiration, runoff, or recharge from 2011–2100 because precipitation is unchanged on average. Increases in extreme event intensity are represented for future conditions producing increased water availability during infrequent events.https://www.mdpi.com/2073-4441/13/1/40climate change riskwatershed water resourcesuncertaintywater balance modelweather generatorMonte Carlo simulation
collection DOAJ
language English
format Article
sources DOAJ
author Nick Martin
spellingShingle Nick Martin
Watershed-Scale, Probabilistic Risk Assessment of Water Resources Impacts from Climate Change
Water
climate change risk
watershed water resources
uncertainty
water balance model
weather generator
Monte Carlo simulation
author_facet Nick Martin
author_sort Nick Martin
title Watershed-Scale, Probabilistic Risk Assessment of Water Resources Impacts from Climate Change
title_short Watershed-Scale, Probabilistic Risk Assessment of Water Resources Impacts from Climate Change
title_full Watershed-Scale, Probabilistic Risk Assessment of Water Resources Impacts from Climate Change
title_fullStr Watershed-Scale, Probabilistic Risk Assessment of Water Resources Impacts from Climate Change
title_full_unstemmed Watershed-Scale, Probabilistic Risk Assessment of Water Resources Impacts from Climate Change
title_sort watershed-scale, probabilistic risk assessment of water resources impacts from climate change
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2021-12-01
description A framework for the assessment of relative risk to watershed-scale water resources from systemic changes is presented. It is composed of two experiments, or pathways, within a Monte Carlo structure and provides quantification of prediction uncertainty. One simulation pathway is the no change, or null hypothesis, experiment, and the other provides simulation of the hypothesized system change. Each pathway uses a stochastic weather generator and a deterministic water balance model. For climate change impact analysis, the framework is calibrated so that the differences between thirty-year average precipitation and temperature pathway values reproduce climate trends. Simulated weather provides forcing for identical water balance models. Probabilistic time histories of differences in actual evapotranspiration, runoff, and recharge provide likelihood per magnitude change to water resources availability. The framework is applied to a semi-arid watershed in Texas. Projected climate trends for the site are a 3 °C increase in average temperature and corresponding increase in potential evapotranspiration, no significant change in average annual precipitation, and a semi-arid classification from 2011–2100. Two types of water balance model are used in separate applications: (1) monthly water balance and (2) daily distributed parameter. Both implementations predict no significant change, on average, to actual evapotranspiration, runoff, or recharge from 2011–2100 because precipitation is unchanged on average. Increases in extreme event intensity are represented for future conditions producing increased water availability during infrequent events.
topic climate change risk
watershed water resources
uncertainty
water balance model
weather generator
Monte Carlo simulation
url https://www.mdpi.com/2073-4441/13/1/40
work_keys_str_mv AT nickmartin watershedscaleprobabilisticriskassessmentofwaterresourcesimpactsfromclimatechange
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