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   https://doi.org/10.1002/2017JD027357  

   Kumar, Rajesh ; Barth, Mary C. ; Pfister, G. G. ; Delle Monache, L. ; Lamarque, J. F. ; Archer-Nicholls, S. ; Tilmes, S. ; Ghude, S. D. ; Wiedinmyer, C. ; Naja, M. ; et al ( February 2018 , Journal of Geophysical Research: Atmospheres)
2. Constructing a long-term monthly climate data set in central Asia: CONSTRUCTING A LONG-TERM MONTHLY CLIMATE DATA SET IN CENTRAL ASIA

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3. Development of late s pring–early summer rainstorms in southern East Asia from the e astward propagating m id‐tropospheric cyclones of South Asia

   https://doi.org/10.1002/joc.7913  

   Chen, Tsing‐Chang ; Tsay, Jenq‐Dar ; Matsumoto, Jun ; Black, Amanda S. ; Chen, Jau‐Ming ( November 2022 , International Journal of Climatology)

   From mid‐May to late June, the eastward propagation of some mid‐tropospheric cyclones (MTCs) originating in the Bay of Bengal (BOB)‐Burma (BUM) region across northern Indochina and southwest China to East Asia are observed. From 1979 to 2016, 137 MTCs were identified for the BOB‐BUM region. Eighty‐eight MTCs were trapped over northern Indochina, but 49 were propagated by the southwesterly flow of the BOB mid‐tropospheric trough to reach East Asia. Thirty‐one moved across Taiwan, but 18 did not. Eventually, all these MTCs moved to Okinawa. The former group of rainstorms produced rainfall ≥100 mm·day⁻¹over Taiwan, while 44 rainstorms generated rainfall ≥50 mm·day⁻¹over Okinawa. The 49 eastward propagating through‐Indochina MTCs exhibited the following salient features: (a) initial formation mostly occurred in the mid‐troposphere ahead/within the BOB trough in the morning over the BOB, but in the afternoon‐evening over BUM. (b) The eastward propagating BOB‐BUM MTCs underwent two descending processes: descending one mandatory level 6 hr after formation, and descending again from 700 to 925 hPa over southeastern China to interact with a low‐level cyclonic shear flow. (c) Intensified (weakened) by dipole anomalous circulation cells, the confluent monsoon southwesterly flow west (east) of Taiwan facilitated the merger of the MTC with a local front. (d) Rainfall produced by rainstorms over Taiwan/Okinawa was maintained by the intensified convergence of water vapour flux toward Taiwan/Okinawa. This hydrological process was stronger toward Taiwan than Okinawa and generated more rainfall in the former region. The impact of the BOB‐BUM MTC on East Asian weather is confirmed by this study.

    

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4. Substantial Increase in the Joint Occurrence and Human Exposure of Heatwave and High‐PM Hazards Over South Asia in the Mid‐21st Century

   https://doi.org/10.1029/2019AV000103  

   Xu, Yangyang ; Wu, Xiaokang ; Kumar, Rajesh ; Barth, Mary ; Diao, Chenrui ; Gao, Meng ; Lin, Lei ; Jones, Bryan ; Meehl, Gerald A. ( June 2020 , AGU Advances)

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5. The Horizontal Slab Beneath East Asia and Its Subdued Surface Dynamic Response

   https://doi.org/10.1029/2020JB021156  

   Liu, Shaofeng ; Ma, Pengfei ; Zhang, Bo ; Gurnis, Michael ( March 2021 , Journal of Geophysical Research: Solid Earth)

   null (Ed.)