Intensification of the Southern Hemisphere summertime subtropical anticyclones in a warming climate

The Southern Hemisphere subtropical anticyclones (SAs) are important features of the Earth's climate. A broad consensus among Coupled Model Intercomparison Project phase 3 and phase 5 climate models suggests an intensification of summer SAs over SH oceans in association with the increase in greenhouse gas concentrations in the atmosphere. Diagnostic and modeling analyses conducted here demonstrate that the strengthening of the SAs is primarily caused by enhanced diabatic heating over continents and cooling over oceans in austral summer. This enhancement of Southern Hemisphere near‐surface SAs identified here together with the enhancement of their Northern Hemisphere counterparts as suggested by Li et al. (2012) indicates increasingly important roles played by SAs in modulating weather and climate on regional and global scales.

[1]  C. Mechoso,et al.  Interhemispheric Influence of the Northern Summer Monsoons on Southern Subtropical Anticyclones , 2013 .

[2]  Y. Kosaka,et al.  Northern Hemisphere Extratropical Tropospheric Planetary Waves and their Low‐Frequency Variability: Their Vertical Structure and Interaction with Transient Eddies and Surface Thermal Contrasts , 2013 .

[3]  Yimin Liu,et al.  Intensification of Northern Hemisphere subtropical highs in a warming climate , 2012 .

[4]  Atmospheric science: Future oceans under pressure , 2012 .

[5]  R. Fu,et al.  Changes to the North Atlantic Subtropical High and Its Role in the Intensification of Summer Rainfall Variability in the Southeastern United States , 2011 .

[6]  H. Nakamura,et al.  Structure and Mechanisms of the Southern Hemisphere Summertime Subtropical Anticyclones , 2010 .

[7]  D. Rahn,et al.  Marine boundary layer over the subtropical southeast Pacific during VOCALS-REx – Part 1: Mean structure and diurnal cycle , 2009 .

[8]  Guoxiong Wu,et al.  Multi-scale forcing and the formation of subtropical desert and monsoon , 2009 .

[9]  C. Deser,et al.  Why the Western Pacific Subtropical High Has Extended Westward since the Late 1970s , 2009 .

[10]  I. Wainer,et al.  The impact of the subtropical South Atlantic SST on South American precipitation , 2008 .

[11]  Brian J. Hoskins,et al.  Impact of Tibetan Orography and Heating on the Summer Flow over Asia(125th Anniversary Issue of the Meteorological Society of Japan) , 2007 .

[12]  H. Nakamura,et al.  Structure and Formation Mechanisms of the Northern Hemisphere Summertime Subtropical Highs , 2005 .

[13]  A. Sterl,et al.  The ERA‐40 re‐analysis , 2005 .

[14]  Yuqing Wang,et al.  Regional Model Simulations of Marine Boundary Layer Clouds over the Southeast Pacific off South America. Part II: Sensitivity Experiments* , 2004 .

[15]  Liu Yimin,et al.  Progress in the study on the formation of the summertime subtropical anticyclone , 2004 .

[16]  Yimin Liu,et al.  Relationship between the Subtropical Anticyclone and Diabatic Heating , 2004 .

[17]  吴国雄,et al.  Progress in the Study on the Formation of the Summertime Subtropical Anticyclone , 2004 .

[18]  Yimin Liu,et al.  Summertime quadruplet heating pattern in the subtropics and the associated atmospheric circulation , 2003 .

[19]  Patrick Minnis,et al.  CIMAR-5: A Snapshot of the Lower Troposphere over the Subtropical Southeast Pacific , 2001 .

[20]  John D. Lenters,et al.  Summertime Precipitation Variability over South America: Role of the Large-Scale Circulation , 1999 .

[21]  R. Elsberry,et al.  Southern Hemisphere Application of the Systematic Approach to Tropical Cyclone Track Forecasting. Part I: Environmental Structure Characteristics , 1997 .

[22]  S. Klein,et al.  The Seasonal Cycle of Low Stratiform Clouds , 1993 .

[23]  Lamont-Doherty Air – Sea Interaction and the Seasonal Cycle of the Subtropical Anticyclones * , 2022 .