Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...

Atmospheric Rivers and Antecedent Soil Moisture


Authors:
Owners: This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource.
Type: Resource
Storage: The size of this resource is 107.6 MB
Created: Apr 17, 2024 at 2:25 p.m.
Last updated: Apr 17, 2024 at 2:54 p.m.
Citation: See how to cite this resource
Sharing Status: Public
Views: 283
Downloads: 4
+1 Votes: Be the first one to 
 this.
Comments: No comments (yet)

Abstract

This repository contains the data and code used to analyze the impact of antecedent soil moisture conditions on flooding caused by atmospheric rivers. Here, we analyze how antecedent soil moisture (ASM) conditions contribute to variability in flood peaks during AR events and how that changes across climatic and physiographic regimes in 122 U.S. West Coast watersheds. We identify a robust non-linear relationship between peak streamflow and ASM during ARs. The inflection point in this relationship represents a watershed-specific critical ASM threshold, above which peak streamflow is, on average, over three times larger. Wet ASM conditions amplify the impacts of more frequent but weaker, lower moisture transport storms, while dry ASM conditions attenuate the flooding that stronger, higher moisture transport events could otherwise cause. Our research shows that watersheds prone to ASM-influenced flooding have higher evaporative indices, lower cold season precipitation, lower snow-to-rain ratios, and shallower, clay-rich soils. Higher evaporation and lower precipitation lead to greater ASM variability during the flood season, increasing flooding during wet periods and buffering flooding during dry periods. Lower snow fraction and shallower soils limit the antecedent water storage capacity of a watershed, contributing to greater sensitivity of flood peaks to ASM variability. Incorporating antecedent moisture condition thresholds into flood models in these regions prone to AR-influenced flooding during ARs could improve forecasts and decrease uncertainty.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Western U.S.
North Latitude
49.5000°
East Longitude
-113.5000°
South Latitude
32.0000°
West Longitude
-125.5000°

Content

Credits

Funding Agencies

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
National Science Foundation Graduate Research Fellowship Program (GRFP) 1937966
Nevada NASA Space Grant Graduate Research Opportunity Fellowship

How to Cite

Webb, M. (2024). Atmospheric Rivers and Antecedent Soil Moisture, HydroShare, http://www.hydroshare.org/resource/0871c3b8775d4153a024f532be34ecd9

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

Comments

There are currently no comments

New Comment

required