Difference between revisions of "Glacial Loading and Tectonics Figure 2"

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[[File:GLTFig2.png|center|1100px]]
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'''Figure 2.'''  
 
'''Figure 2.'''  
 
Maximum ice extent during the Last Glacial Maximum (at 18,900 years BP) modeled using the University of Maine Ice Sheet Model (UMISM) for the last glacial (~116 ka). Base precipitation and temperature grids are hybrid, derived from WorldClim (Hijmans et al. 2005) over land areas, and NCEP/NCAR Reanalysis (Kalnay et al., 1996) over ocean areas. The annual averages for both WorldClim and NCEP precipitation and temperature used for base climate (http://cci-reanalyzer.org, Personal communication, Sean Birkel).
 
Maximum ice extent during the Last Glacial Maximum (at 18,900 years BP) modeled using the University of Maine Ice Sheet Model (UMISM) for the last glacial (~116 ka). Base precipitation and temperature grids are hybrid, derived from WorldClim (Hijmans et al. 2005) over land areas, and NCEP/NCAR Reanalysis (Kalnay et al., 1996) over ocean areas. The annual averages for both WorldClim and NCEP precipitation and temperature used for base climate (http://cci-reanalyzer.org, Personal communication, Sean Birkel).

Latest revision as of 15:46, 18 March 2015

GLTFig2.png

Figure 2. Maximum ice extent during the Last Glacial Maximum (at 18,900 years BP) modeled using the University of Maine Ice Sheet Model (UMISM) for the last glacial (~116 ka). Base precipitation and temperature grids are hybrid, derived from WorldClim (Hijmans et al. 2005) over land areas, and NCEP/NCAR Reanalysis (Kalnay et al., 1996) over ocean areas. The annual averages for both WorldClim and NCEP precipitation and temperature used for base climate (http://cci-reanalyzer.org, Personal communication, Sean Birkel).