Impact of Dust-Cloud-Radiation-Precipitation Dynamical Feedback on Subseasonal-to-Seasonal Variability of the Asian Summer Monsoon in Global Variable-Resolution Simulations With MPAS-CAM5

Lau, William K. M.; Kim, Kyu-Myong; Zhao, Chun; Leung, L. Ruby; Park, Sang-Hun

doi:10.3389/feart.2020.00226

Title: Impact of Dust-Cloud-Radiation-Precipitation Dynamical Feedback on Subseasonal-to-Seasonal Variability of the Asian Summer Monsoon in Global Variable-Resolution Simulations With MPAS-CAM5

Journal Article · Fri Jun 19 00:00:00 EDT 2020 · Frontiers in Earth Science

DOI:https://doi.org/10.3389/feart.2020.00226· OSTI ID:1863892

Lau, William K. M. ^[1]; Kim, Kyu-Myong ^[2]; Zhao, Chun ^[3];

^[4]; Park, Sang-Hun ^[5]

Univ. of Maryland, College Park, MD (United States)
NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States)
Univ. of Science and Technology of China, Hefei (China)
Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
Yonsei Univ., Seoul (Korea, Republic of)

In this study, we investigate the effects of increased dust emission from the Middle East deserts on subseasonal-to-seasonal (S₂S) variability of the Asian summer monsoon (ASM). Numerical experiments are performed using the Model for Prediction Across Scales (MPAS) coupled with the Community Atmosphere Model (CAM5) physics, with regional refinement at 30 km grid resolution over South Asia and the surrounding regions. Result shows that increased dust emission and transport from the Middle East/West Asia region induces a strong dust-cloud-radiation-precipitation-circulation feedback, resulting in a colder surface over the desert regions and the western Tibetan Plateau, but warmer and moister troposphere with enhanced cloudiness and precipitation over the Pakistan/Northwest India (PNWI) region. The latter changes are amplified by the dust aerosol induced Elevated Heat Pump (EHP) mechanism along the West Himalayas/Iranian Plateau foothill regions, most pronounced during May-June. During July-August, cloud radiation feedback further enhances the warming of the upper troposphere, and cooling of the land surface over the PNWI and adjacent regions over West Asia. The upper tropospheric heating and increased precipitation over PNWI spur a large-scale anomalous Rossby wavetrain and a northward displacement of the subtropical jetstream, manifesting in a contraction of the South Asian High and westward shift of the Western Pacific Subtropical High. As a result, the entire ASM precipitation-cloud system is displaced westward. Precipitation and cloudiness are intensified over northwest and western India and west Asia, but suppressed over southern and central East Asia. Analyses of the S₂S variability of the upper level vorticity balance suggests that heating by Middle East dust plays an important role in exciting, and anchoring a teleconnection pattern through interactions among dust-cloud radiation, precipitation heating over the PNWI, the development of an upper level Rossby wavetrain, and the northward shift of the boreal summer jetstream over Eurasia.

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Research Organization:: Pacific Northwest National Lab. (PNNL), Richland, WA (United States)

Sponsoring Organization:: USDOE Office of Science (SC), Biological and Environmental Research (BER); Central Universities of China; National Natural Science Foundation of China (NSFC)

Grant/Contract Number:: AC05-76RL01830; 300426-00001; 41775146

OSTI ID:: 1863892

Report Number(s):: PNNL-SA-155707

Journal Information:: Frontiers in Earth Science, Vol. 8; ISSN 2296-6463

Publisher:: Frontiers Research FoundationCopyright Statement

Country of Publication:: United States

Language:: English

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Title: Impact of Dust-Cloud-Radiation-Precipitation Dynamical Feedback on Subseasonal-to-Seasonal Variability of the Asian Summer Monsoon in Global Variable-Resolution Simulations With MPAS-CAM5

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