In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 46, No. 5 ( 2019-03-16), p. 2911-2921
Abstract:
Tropical upward motion exhibits a bimodal diurnal cycle with a top‐heavy shape during the day and a bottom‐heavy shape at night The diurnal radiative heating cycle within anvil clouds is critical to upper‐level diurnal circulation change Upper‐level lifting due to daytime cloud‐shortwave heating causes an afternoon peak in anvil clouds, indicating a feedback
Type of Medium:
Online Resource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2018GL081806
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2021599-X
detail.hit.zdb_id:
7403-2
SSG:
16,13
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