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NCA-LDAS: Overview and Analysis of Hydrologic Trends for the National Climate Assessment

Authors :
Michael F. Jasinski
Jordan S. Borak
Sujay V. Kumar
David M. Mocko
Christa D. Peters-Lidard
Matthew Rodell
Hualan Rui
Hiroko K. Beaudoing
Bruce E. Vollmer
Kristi R. Arsenault
Bailing Li
John D. Bolten
Natthachet Tangdamrongsub
Source :
Journal of Hydrometeorology. 20(8)
Publication Year :
2019
Publisher :
United States: NASA Center for Aerospace Information (CASI), 2019.

Abstract

Terrestrial hydrologic trends over the conterminous United States are estimated for 1980–2015 using the National Climate Assessment Land Data Assimilation System (NCA-LDAS) reanalysis. NCA-LDAS employs the uncoupled Noah version 3.3 land surface model at 0.125° 3 0.125° forced with NLDAS-2 meteorology, rescaled Climate Prediction Center precipitation, and assimilated satellite-based soil moisture, snow depth, and irrigation products. Mean annual trends are reported using the nonparametric Mann–Kendall test at p < 0.1 significance. Results illustrate the interrelationship between regional gradients in forcing trends and trends in other land energy and water stores and fluxes. Mean precipitation trends range from +3 to +9 mm/yr in the upper Great Plains and Northeast to -1 to -9 mm/yr in the West and South, net radiation flux trends range from +0.05 to +0.20 W/sq. m yr in the East to -0.05 to -0.20 W/sq. m yr in the West, and U.S.-wide temperature trends average about +0.03K/yr. Trends in soil moisture, snow cover, latent and sensible heat fluxes, and runoff are consistent with forcings, contributing to increasing evaporative fraction trends from west to east. Evaluation of NCA-LDAS trends compared to independent data indicates mixed results. The RMSE of U.S.-wide trends in number of snow cover days improved from 3.13 to 2.89 days/yr while trend detection increased 11%. Trends in latent heat flux were hardly affected, with RMSE decreasing only from 0.17 to 0.16 W/sq. m yr, while trend detection increased 2%. NCA-LDAS runoff trends degraded significantly from 2.6 to 16.1 mm/yr while trend detection was unaffected. Analysis also indicated that NCA-LDAS exhibits relatively more skill in low precipitation station density areas, suggesting there are limits to the effectiveness of satellite data assimilation in densely gauged regions. Overall, NCA-LDAS demonstrates capability for quantifying physically consistent, U.S. hydrologic climate trends over the satellite era.

Details

Language :
English
ISSN :
15257541 and 1525755X
Volume :
20
Issue :
8
Database :
NASA Technical Reports
Journal :
Journal of Hydrometeorology
Notes :
281945.02.80.01.50
Publication Type :
Report
Accession number :
edsnas.20210012710
Document Type :
Report
Full Text :
https://doi.org/10.1175/JHM-D-17-0234.1