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Assimilating multi-satellite snow data in ungauged Eurasia improves the simulation accuracy of Asian monsoon seasonal anomalies

Bibliographic Data

ID15545644
AuthorsPeirong Lin (0000-0002-7275-7470, The University of Texas at Austin, corresponding author), Zong‐Liang Yang (0000-0003-3030-0330, Chinese Academy of Sciences), Jiangfeng Wei (0000-0001-8981-8674, Nanjing University of Information Science and Technology), Robert E Dickinson (0000-0002-8352-4517, The University of Texas at Austin), Yongfei Zhang (0000-0001-8777-6642, Princeton University), Long Zhao (0000-0002-1012-0159, Southwest University)
Year2020
Volume15
Issue6
Pages064033-064033
Publication date2020-03-18
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ab80ef
OpenAlexW3012335232
LanguageEN
References cited2

Properly initializing land snow conditions with multi-satellite data assimilation (DA) may help tackle the long-standing challenge of Asian monsoon seasonal forecasts. However, to what extent can snow DA help resolve the problem remains largely unexplored. Here we establish, for the first time, that improved springtime snow initializations assimilating the Moderate Spectral Imaging Satellite (MODIS) snow cover fraction and the Gravity Recovery and Climate Experiment (GRACE) terrestrial water storage data can improve the simulation accuracy of Asian monsoon seasonal anomalies. Focusing on the western Tibetan Plateau (TP) and mid- to high-latitude Eurasia (EA), two regions where multi-satellite snow DA is critical, we found that DA influences the monsoon circulation at different months depending on the regional snow–atmosphere coupling strengths. For the pre-monsoon season, accurate initialization of the TP snow is key, and assimilating MODIS data slightly outperforms jointly assimilating MODIS and GRACE data. For the peak-monsoon season, accurate initialization of the EA snow is more important due to its long memory, and assimilating GRACE data brings the most pronounced gains. Among all the Asian monsoon subregions, the most robust improvement is seen over central north India, a likely result of the region’s strong sensitivity to thermal forcing. While this study highlights complementary snow observations as promising new sources of the monsoon predictability, it also clarifies complexities in translating DA to useful monsoon forecast skill, which may help bridge the gap between land DA and dynamical climate forecasting studies

Climatology · Data assimilation · East Asian Monsoon · Forcing (mathematics · Geography · Initialization · Meteorology · Monsoon · Monsoon of South Asia · Plateau (mathematics · Predictability · Satellite · Snow · Climate variability and models · Computer Science · Cryospheric studies and observations · Environmental Science · Geophysics and Gravity Measurements · Geology

  • Seasonal climate predictability and forecasting

    Open Access•Francisco J Doblas‐Reyes, Javier García‐Serrano et al.•Wiley Interdisciplinary Reviews…•2013

Citation velocityhistorical
Highly citedNo

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