Global climate evolution during the last deglaciation

Deciphering the evolution of global climate from the end of the Last Glacial Maximum approximately 19 ka to the early Holocene 11 ka presents an outstanding opportunity for understanding the transient response of Earth’s climate system to external and internal forcings. During this interval of globa...

Täydet tiedot

Tallennettuna:
Bibliografiset tiedot
Päätekijät: Clark, Peter U., Shakun, Jeremy D., Baker, Paul A., Bartlein, Patrick J., Brewer, Simon, Brook, Ed, Carlson, Anders E., Cheng, Hai, Kaufman, Darrell S., Liu, Zhengyu, Marchitto, Thomas M., Mix, Alan C., Morrill, Carrie, Otto-Bliesner, Bette L., Pahnke, Katharina, Russell, James M., Whitlock, Cathy, Adkins, Jess F., Blois, Jessica L., Clark, Jorie, Colman, Steven M., Curry, William B., Flower, Ben P., He, Feng, Johnson, Thomas C., Lynch-Stieglitz, Jean, Markgraf, Vera, McManus, Jerry, Mitrovica, Jerry X., Moreno, Patricio I., Williams, John W.
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: National Academy of Sciences 2012
Aiheet:
PNAS Plus
Linkit:https://ncbi.nlm.nih.gov/pmc/articles/PMC3358890/
https://ncbi.nlm.nih.gov/pubmed/22331892
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1116619109
Tagit: Lisää tagi
Ei tageja, Lisää ensimmäinen tagi!

Samankaltaisia teoksia