FN Archimer Export Format
PT J
TI Dipole patterns in tropical precipitation were pervasive across landmasses throughout Marine Isotope Stage 5
BT 
AF Nilsson-Kerr, Katrina
   Anand, Pallavi
   Holden, Philip B.
   Clemens, Steven C.
   Leng, Melanie J.
AS 1:1;2:1;3:1;4:2;5:3,4;
FF 1:;2:;3:;4:;5:;
C1 Faculty of STEM, School of Environment, Earth and Ecosystem Sciences, The Open University, Milton Keynes, UK
   Department of Geological Sciences, Brown University, Providence, RI, USA
   National Environmental Isotope Facility, British Geological Survey, Nottingham, UK
   School of Biosciences, University of Nottingham, Loughborough, UK
C2 UNIV OPEN, UK
   UNIV BROWN, USA
   BRITISH GEOL SURVEY, UK
   UNIV NOTTINGHAM, UK
IF 7.29
TC 8
UR https://archimer.ifremer.fr/doc/00685/79705/82497.pdf
   https://archimer.ifremer.fr/doc/00685/79705/82498.pdf
   https://archimer.ifremer.fr/doc/00685/79705/82499.pdf
   https://archimer.ifremer.fr/doc/00685/79705/82500.xlsx
LA English
DT Article
CR IMAGES 4-MD111
   MD 119 / TIP 2000
   MD 126 / MONA
   MD 148 / PECTEN
   MD 155 / MARCO-POLO2
   MD 167 / RETRO (IMAGES XVI)
   MOZAPHARE-MD104
   NAUSICAA-IMAGES 2-MD105
BO Marion Dufresne
AB Most of Earth’s rain falls in the tropics, often in highly seasonal monsoon rains, which are thought to be coupled to the inter-hemispheric migrations of the Inter-Tropical Convergence Zone in response to the seasonal cycle of insolation. Yet characterization of tropical rainfall behaviour in the geologic past is poor. Here we combine new and existing hydroclimate records from six large-scale tropical regions with fully independent model-based rainfall reconstructions across the last interval of sustained warmth and ensuing climate cooling between 130 to 70 thousand years ago (Marine Isotope Stage 5). Our data-model approach reveals large-scale heterogeneous rainfall patterns in response to changes in climate. We note pervasive dipole-like tropical precipitation patterns, as well as different loci of precipitation throughout Marine Isotope Stage 5 than recorded in the Holocene. These rainfall patterns cannot be solely attributed to meridional shifts in the Inter-Tropical Convergence Zone. 
PY 2021
PD MAR
SO Communications Earth & Environment
SN 2662-4435
PU Springer Science and Business Media LLC
VL 2
IS 1
UT 000665768900005
DI 10.1038/s43247-021-00133-7
ID 79705
ER

EF