Evolution of the meridional shift of the subtropical and subpolar westerly jet over the Southern Hemisphere during the past 21,000 years-Reference-Cited by-同舟云学术

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Evolution of the meridional shift of the subtropical and subpolar westerly jet over the Southern Hemisphere during the past 21,000 years

Published:2020-10 Issue: Volume:246 Page:106544
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Jiang Nanxuan,Yan Qing

Funder

National Key Research and Development Program of China

Chinese Academy of Sciences

Youth Innovation Promotion Association by CAS

Publisher

Elsevier BV

Subject

Geology,Archaeology,Archaeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference57 articles.

1. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2;Anderson;Science,2009

2. Change in future climate due to Antarctic meltwater;Bronselaer;Nature,2018

3. Greenland-wide seasonal temperatures during the last deglaciation;Buizert;Geophys. Res. Lett.,2018

4. The relationship between the ITCZ and the Southern Hemispheric eddy-driven jet;Ceppi;J. Geophys. Res.: Atmospheres,2013

5. Southern westerlies in LGM and future (RCP4.5) climates;Chavaillaz;Clim. Past,2013

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1. The North Atlantic subpolar ocean dynamics during the past 21,000 years;Dynamics of Atmospheres and Oceans;2024-06

2. Modeling the timing of Patagonian Ice Sheet retreat in the Chilean Lake District from 22–10 ka;The Cryosphere;2024-03-26

3. Southward shifts and enhancements of the westerlies over the Tibetan Plateau during North Atlantic cooling events;Quaternary Science Reviews;2024-01

4. Glacial-Interglacial Changes in Antarctic Intermediate Water Advection in the Southeast Pacific During the Last 787 Kyr;2024

5. Modeling the effects of global cooling and the Tethyan Seaway closure on North African and South Asian climates during the Middle Miocene Climate Transition;Palaeogeography, Palaeoclimatology, Palaeoecology;2023-06

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