Role of cloud feedback in regulating the “pool of inhibited cloudiness” over the Bay of Bengal View Full Text


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Article Info

DATE

2019-04

AUTHORS

Anish Kumar M. Nair, T. Narayana Rao, K. Rajeev

ABSTRACT

Cloud-circulation feedback by latent heating (LH) is a major contributor for driving atmospheric circulation. This study examines the potential role of spatial variations of LH in driving a mini-circulation for generating the “pool of inhibited cloudiness”, where cloud formation in the lower and middle troposphere is significantly inhibited over the southwest Bay of Bengal (BoB) during the Indian summer monsoon. Spaceborne observations show that LH rates in the deep convective regions of the head BoB are as high as 0.2 K/h, while that over the “pool” are about 5 times smaller. This differential heating results in modulating the mean circulation. 20 years of reanalysis data show good correlation between (a) upper troposphere (300 hPa) convergence and lower tropospheric (1000 hPa) divergence at the “pool” and (b) lower tropospheric divergence at the “pool” and lower tropospheric convergence at the head BoB as well as at the west coast of India. Besides the orographic influence, a portion of the air mass descending at the “pool” arises from deep convective regions in the north BoB and equatorial trough. This subsidence is responsible for the persistent inhibition to cloud formation at the “pool”. This case forms a classic example of the cloud-circulation feedback. More... »

PAGES

183-194

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/s00703-017-0560-7

DOI

http://dx.doi.org/10.1007/s00703-017-0560-7

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https://app.dimensions.ai/details/publication/pub.1092239591


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