Drier tropical and subtropical Southern Hemisphere in the mid-Pliocene Warm Period

Thermodynamic arguments imply that global mean rainfall increases in a warmer atmosphere; however, dynamical effects may result in more significant diversity of regional precipitation change. Here we investigate rainfall changes in the mid-Pliocene Warm Period (~ 3 Ma), a time when temperatures were...

Täydet tiedot

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Bibliografiset tiedot
Julkaisussa:Sci Rep
Päätekijät: Pontes, Gabriel M., Wainer, Ilana, Taschetto, Andréa S., Sen Gupta, Alex, Abe-Ouchi, Ayako, Brady, Esther C., Chan, Wing-Le, Chandan, Deepak, Contoux, Camille, Feng, Ran, Hunter, Stephen J., Kame, Yoichi, Lohmann, Gerrit, Otto-Bliesner, Bette L., Peltier, W. Richard, Stepanek, Christian, Tindall, Julia, Tan, Ning, Zhang, Qiong, Zhang, Zhongshi
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: Nature Publishing Group UK 2020
Aiheet:
Article
Linkit:https://ncbi.nlm.nih.gov/pmc/articles/PMC7417591/
https://ncbi.nlm.nih.gov/pubmed/32778702
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-020-68884-5
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