Daily Precipitation Frequency Distributions Impacts on Land-Surface Simulations of CONUS

Many precipitation-driven data products from land data assimilation systems support assessments of droughts, floods, and other societally-relevant land-surface processes. The accumulated precipitation used as input to these products has a significant impact on water budgets; however, the effects of...

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Main Authors: Daniel P. Sarmiento, Kimberly Slinski, Amy McNally, Jossy P. Jacob, Chris Funk, Pete Peterson, Christa D. Peters-Lidard
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-08-01
Series:Frontiers in Water
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/frwa.2021.640736/full
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author Daniel P. Sarmiento
Daniel P. Sarmiento
Kimberly Slinski
Kimberly Slinski
Amy McNally
Amy McNally
Jossy P. Jacob
Jossy P. Jacob
Chris Funk
Pete Peterson
Christa D. Peters-Lidard
author_facet Daniel P. Sarmiento
Daniel P. Sarmiento
Kimberly Slinski
Kimberly Slinski
Amy McNally
Amy McNally
Jossy P. Jacob
Jossy P. Jacob
Chris Funk
Pete Peterson
Christa D. Peters-Lidard
author_sort Daniel P. Sarmiento
collection DOAJ
description Many precipitation-driven data products from land data assimilation systems support assessments of droughts, floods, and other societally-relevant land-surface processes. The accumulated precipitation used as input to these products has a significant impact on water budgets; however, the effects of daily distribution of precipitation on these products are not well known. A comparison of the Integrated Multi-satellite Retrievals for GPM (IMERG) and Climate Hazards Group InfraRed Precipitation with Stations version 2 (CHIRPS2) rainfall products over the continental United States (CONUS) was performed to quantify the impacts of the daily distribution of precipitation on biases and errors in soil moisture, runoff, and evapotranspiration (ET). Since the total accumulated precipitation between the IMERG and CHIRPS product differed, a third precipitation product, CHIRPS-to-IMERG (CHtoIM), was produced that used CHIRPS2 accumulated precipitation totals and the daily precipitation frequency distribution of IMERG. This new product supported a controlled analysis of the impact of precipitation frequency distribution on simulated hydrological fields. The CHtoIM had higher occurrences of precipitation in the 0–5 mm day−1 range, with a lower occurrence of dry days, which decreased soil moisture and surface runoff in the land-surface model. The surface soil layer had a tendency to reach saturation more often in the CHIRPS2 simulations, where the number of moderate to heavy precipitation days (>5 mm day−1) was increased. Using the blended CHtoIM product as input reduced errors in surface soil moisture by 5–15% when compared to Soil Moisture Active/Passive (SMAP) data. Similarly, ET errors were also slightly decreased (~2%) when compared to SSEBop data. Moderate changes in daily precipitation distributions had a quantifiable impact on soil moisture, runoff, and ET. These changes usually improved the model when compared to other modeled and observational datasets, but the magnitude of the improvements varied by region and time of year.
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spelling doaj.art-c43e119aa38a47eea691804d03c1860e2022-12-21T22:12:11ZengFrontiers Media S.A.Frontiers in Water2624-93752021-08-01310.3389/frwa.2021.640736640736Daily Precipitation Frequency Distributions Impacts on Land-Surface Simulations of CONUSDaniel P. Sarmiento0Daniel P. Sarmiento1Kimberly Slinski2Kimberly Slinski3Amy McNally4Amy McNally5Jossy P. Jacob6Jossy P. Jacob7Chris Funk8Pete Peterson9Christa D. Peters-Lidard10Hydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, United StatesSAIC, Inc., McLean, VA, United StatesHydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, United StatesUniversity of Maryland Earth Systems Science Interdisciplinary Center, College Park, MD, United StatesSAIC, Inc., McLean, VA, United StatesUnited States Agency for International Development, Washington, DC, United StatesHydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, United StatesSSAI, Inc., Lanham, MD, United StatesDepartment of Geography and Climate Hazards Center, University of California, Santa Barbara, Santa Barbara, CA, United StatesDepartment of Geography and Climate Hazards Center, University of California, Santa Barbara, Santa Barbara, CA, United StatesHydrological Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, United StatesMany precipitation-driven data products from land data assimilation systems support assessments of droughts, floods, and other societally-relevant land-surface processes. The accumulated precipitation used as input to these products has a significant impact on water budgets; however, the effects of daily distribution of precipitation on these products are not well known. A comparison of the Integrated Multi-satellite Retrievals for GPM (IMERG) and Climate Hazards Group InfraRed Precipitation with Stations version 2 (CHIRPS2) rainfall products over the continental United States (CONUS) was performed to quantify the impacts of the daily distribution of precipitation on biases and errors in soil moisture, runoff, and evapotranspiration (ET). Since the total accumulated precipitation between the IMERG and CHIRPS product differed, a third precipitation product, CHIRPS-to-IMERG (CHtoIM), was produced that used CHIRPS2 accumulated precipitation totals and the daily precipitation frequency distribution of IMERG. This new product supported a controlled analysis of the impact of precipitation frequency distribution on simulated hydrological fields. The CHtoIM had higher occurrences of precipitation in the 0–5 mm day−1 range, with a lower occurrence of dry days, which decreased soil moisture and surface runoff in the land-surface model. The surface soil layer had a tendency to reach saturation more often in the CHIRPS2 simulations, where the number of moderate to heavy precipitation days (>5 mm day−1) was increased. Using the blended CHtoIM product as input reduced errors in surface soil moisture by 5–15% when compared to Soil Moisture Active/Passive (SMAP) data. Similarly, ET errors were also slightly decreased (~2%) when compared to SSEBop data. Moderate changes in daily precipitation distributions had a quantifiable impact on soil moisture, runoff, and ET. These changes usually improved the model when compared to other modeled and observational datasets, but the magnitude of the improvements varied by region and time of year.https://www.frontiersin.org/articles/10.3389/frwa.2021.640736/fullland-surface modelhydrologyprecipitationLISsoil moisture
spellingShingle Daniel P. Sarmiento
Daniel P. Sarmiento
Kimberly Slinski
Kimberly Slinski
Amy McNally
Amy McNally
Jossy P. Jacob
Jossy P. Jacob
Chris Funk
Pete Peterson
Christa D. Peters-Lidard
Daily Precipitation Frequency Distributions Impacts on Land-Surface Simulations of CONUS
Frontiers in Water
land-surface model
hydrology
precipitation
LIS
soil moisture
title Daily Precipitation Frequency Distributions Impacts on Land-Surface Simulations of CONUS
title_full Daily Precipitation Frequency Distributions Impacts on Land-Surface Simulations of CONUS
title_fullStr Daily Precipitation Frequency Distributions Impacts on Land-Surface Simulations of CONUS
title_full_unstemmed Daily Precipitation Frequency Distributions Impacts on Land-Surface Simulations of CONUS
title_short Daily Precipitation Frequency Distributions Impacts on Land-Surface Simulations of CONUS
title_sort daily precipitation frequency distributions impacts on land surface simulations of conus
topic land-surface model
hydrology
precipitation
LIS
soil moisture
url https://www.frontiersin.org/articles/10.3389/frwa.2021.640736/full
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