'Lgm' presentation slideshows

LGM Seasonal Energetics

LGM Seasonal Energetics. October, 2009. Annual mean insolation. Reflects Obliquity Change Only (Modern = 23.45 LGM = 22.95). TOA seasonal incoming Insolation. Primarily reflects obliquity (precession change from 102 in modern to 114 in LGM), biggest high latitude effect in summer.

706 views • 62 slides

Lecture 14: The LGM (Last Glacial Maximum)

Lecture 14: The LGM (Last Glacial Maximum). Part III: Deglacial and Millennial Climate Changes. (Chapter 12). Last Glacial Maximum. Big signal. 21,000. Much more data, with 14 C dating. Mammals of the Last Glacial Maximum (21,000 years ago). Cave painting of LGM era in Southern France.

609 views • 49 slides

LGM Seasonal Energetics

LGM Seasonal Energetics. October, 2009. Annual mean insolation. Reflects Obliquity Change Only (Modern = 23.45 LGM = 22.95). TOA seasonal incoming Insolation. Primarily reflects obliquity (precession change from 102 in modern to 114 in LGM), biggest high latitude effect in summer.

500 views • 40 slides

LGM Seasonal Energetics

LGM Seasonal Energetics. October, 2009. Annual mean insolation. Reflects Obliquity Change Only (Modern = 23.45 LGM = 22.95). TOA seasonal incoming Insolation. Primarily reflects obliquity (precession change from 102 in modern to 114 in LGM), biggest high latitude effect in summer.

405 views • 40 slides

South American Climate of the LGM: A Regional Modeling Study

537 views • 37 slides

Marisa Montoya 1 , Anders Levermann 2, 3, Andreas Born 4,5

501 views • 36 slides

(1) BRIDGE, School of Geographical Sciences, University of Bristol, UK

Transient simulations of the last 30,000 years, within the GENIE earth-system framework D.J. Lunt (1) M.Williamson (2) A. Price (3) P.J. Valdes (1). What is GENIE? Energy-balance-atmosphere transient coupled simulations Fully-dynamic-atmosphere transient slab simulations

178 views • 17 slides

Coupled model

An altered atmospheric circulation regime during Last Glacial Maximum Camille Li, Aaron Donohoe David Battisti University of Washington. Coupled model. winter jet and storminess. poleward heat flux 850mb (Km/s). Coupled model. winter jet and storminess.

230 views • 7 slides

Coupled model

An altered atmospheric circulation regime during Last Glacial Maximum Camille Li, Aaron Donohoe David Battisti University of Washington. Coupled model. winter jet and storminess. poleward heat flux 850mb (Km/s). Coupled model. winter jet and storminess.

72 views • 7 slides

Delayed onset of the South American Monsoon during the Last Glacial Maximum

Delayed onset of the South American Monsoon during the Last Glacial Maximum. Kerry H. Cook and Edward K. Vizy, Cornell University. I. INTRODUCTION

146 views • 1 slides