Factors controlling Hadley circulation changes from the Last Glacial Maximum to the end of the 21st century-Reference-Cited by-同舟云学术

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Factors controlling Hadley circulation changes from the Last Glacial Maximum to the end of the 21st century

Published:2017-08-28 Issue:16 Volume:44 Page:8585-8591
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

D'Agostino Roberta¹²³,Lionello Piero²³^ORCID,Adam Ori⁴⁵^ORCID,Schneider Tapio⁴⁶^ORCID

Affiliation:

1. Max Planck Institute for Meteorology; Hamburg Germany

2. DiSTeBA; University of Salento; Lecce Italy

3. Euro-Mediterranean Center on Climate Change; Lecce Italy

4. Geological Institute; ETH Zurich; Switzerland

5. Hebrew University; Jerusalem Israel

6. California Institute of Technology; Pasadena California USA

Funder

Università del Salento

JPI Climate-Belmont Forum project

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017GL074533/fullpdf

Reference30 articles.

1. Role of changes in mean temperatures versus temperature gradients in the recent widening of the Hadley circulation;Adam;J. Clim.,2014

2. Recent widening of the tropical belt from global tropopause statistics: Sensitivities;Birner;J. Geophys. Res.,2010

3. Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum-Part 1: Experiments and large-scale features;Braconnot;Clim. Past,2007

4. Extratropical cooling, interhemispheric thermal gradients, and tropical climate change;Chiang;Annu. Rev. Earth Planet. Sci.,2012

5. Evidence of global warming impact on the evolution of the Hadley circulation in ECMWF centennial reanalyses;D'Agostino;Clim. Dyn.,2017

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