In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 50, No. 13 ( 2023-07-16)
Abstract:
A unique rainfall record in the Thai‐Malay and a transient simulation suggest a summer to winter rainfall regime shift during the Holocene Transient paleoclimate simulation simulation reveals that this shift was caused by westward migration of the boundary between summer and winter rainfall regimes This regime shift could occur in regions around the boundaries of rainfall regimes in the tropics and possibly worldwide
Type of Medium:
Online Resource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2023GL102909
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2023
detail.hit.zdb_id:
2021599-X
detail.hit.zdb_id:
7403-2
SSG:
16,13