[2012-03-25] Broad range of 2050 warming from an observationally constrained large climate model ensemble

Broad range of 2050 warming from an observationally constrained large climate model ensemble  

Publication Date:  2012-03-25
Creator:  Matthew Collins
Myles R. Allen
Daniel J. Rowlands
David J. Frame
Duncan Ackerley
Tolu Aina
Ben B.B. Booth
Carl Christensen
Nicholas Faull
Chris E. Forest
Benjamin S. Grandey
Edward Gryspeerdt
Eleanor J. Highwood
William J. Ingram
Sylvia Knight
Ana Lopez
Neil Massey
Frances McNamara
Nicolai Meinshausen
Claudio Piani
Suzanne M. Rosier
Benjamin M. Sanderson
Leonard A. Smith
Daithi A. Stone
Milo Thurston
Kuniko Yamazaki
Y. Hiro Yamazaki
Publisher.Display:  Macmillan Publishers Limited
Subjects.Display:  Climate change
Greenhouse gases
temperature changes,global
Earth (Planet)--Surface temperature
Source Institution:  Florida International University
[2012-03-25] Broad range of 2050 warming from an observationally constrained large climate model ensemble
[2013-09] El Nino modulations over the past centuries

El Nino modulations over the past centuries  

Publication Date:  2013-09
Creator:  Jianbao Li
Shang-Ping Xie
Edward R. Cook
Mariano S. Morales
Duncan R. Christie
Nathaniel C. Johnson
Fahu Chen
Rosanne D'Arrigo
Anthony M. Fowler
Xiaohua Gou
Keyan Fang
Publisher.Display:  Macmillan Publishers Limited
Subjects.Display:  Climate change
Northern Hemisphere
Pacific area
unknownEl Nino current
Source Institution:  Florida International University
[2013-09] El Nino modulations over the past centuries
[2014] Evidence for elevated and spatially variable geothermal flux beneath the West Antarctic Ice Sheet

Evidence for elevated and spatially variable geothermal flux beneath the West Antarctic Ice Sheet  

Publication Date:  2014
Creator:  Quartini, Enrica
Young, Duncan A.
Schroeder, Dustin M.
Blankenship, Donald D.
Publisher.Display:  National Academy of Sciences
Subjects.Display:  Climate change
ice sheets
Antarctica
glaciers
Source Institution:  Florida International University
[2014] Evidence for elevated and spatially variable geothermal flux beneath the West Antarctic Ice Sheet