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Revisiting the physical processes controlling the tropical atmospheric circulation changes during the Mid-Piacenzian Warm Period

Zhang, Ke (author)
Sun, Yong (author)
Zhang, Zhongshi (author)
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Stepanek, Christian (author)
Feng, Ran (author)
Hill, Daniel (author)
Lohmann, Gerrit (author)
Dolan, Aisling (author)
Haywood, Alan (author)
Abe-Ouchi, Ayako (author)
Otto-Bliesner, Bette (author)
Contoux, Camille (author)
Chandan, Deepak (author)
Ramstein, Gilles (author)
Dowsett, Harry (author)
Tindall, Julia (author)
Baatsen, Michiel (author)
Tan, Ning (author)
Peltier, William Richard (author)
Li, Qiang (author)
Stockholms universitet,Institutionen för naturgeografi,Bolincentret för klimatforskning (tills m KTH & SMHI)
Chan, Wing-Le (author)
Wang, Xin (author)
Zhang, Xu (author)
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 (creator_code:org_t)
2024
2024
English.
In: Quaternary International. - 1040-6182 .- 1873-4553. ; 682, s. 46-59
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • The Mid-Piacenzian Warm Period (MPWP; 3.0–3.3 Ma), a warm geological period about three million years ago, has been deemed as a good past analog for understanding the current and future climate change. Based on 12 climate model outputs from Pliocene Model Intercomparison Project Phase 2 (PlioMIP2), we investigate tropical atmospheric circulation (TAC) changes under the warm MPWP and associated underlying mechanisms by diagnosing both atmospheric static stability and diabatic processes. Our findings underscore the advantage of analyzing atmospheric diabatic processes in elucidating seasonal variations of TAC compared to static stability assessments. Specifically, by diagnosing alterations in diabatic processes, we achieve a quantitative understanding and explanation the following TAC changes (incl. Strength and edge) during the MPWP: the weakened (annual, DJF, JJA) Northern Hemisphere and (DJF) Southern Hemisphere Hadley circulation (HC), reduced (annual, DJF) Pacific Walker circulation (PWC) and enhanced (annual, JJA) Southern Hemisphere HC and (JJA) PWC, and westward shifted (annual, DJF, JJA) PWC. We further addressed that the increasing bulk subtropical static stability and/or decreasing vertical shear of subtropical zonal wind - two crucial control factors for changes in subtropical baroclinicity - may promote HC widening, and vice versa. Consequently, our study of spatial diabatic heating and cooling, corresponding to upward and downward motions within the TAC, respectively, provides a new perspective for understanding the processes controlling seasonal TAC changes in response to surface warming.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)

Keyword

Pliocene
PlioMIP2
Hadley circulation
Walker circulation
Diabatic heating/cooling
Subtropical baroclinicity

Publication and Content Type

ref (subject category)
art (subject category)

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