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METEOROLOGY

METEOROLOGY. GEL-1370. Chapter Fourteen. Climate Change. Goal for this Chapter. We are going to learn answers to the following questions: How the global climate has changed in the past Theories on why the global climate has changed?.

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555 views • 40 slides

Transient (monsoonal) climate behavior in CLIMBER

Transient (monsoonal) climate behavior in CLIMBER. Erik Tuenter Faculty of Geosciences, Utrecht University, The Netherlands Royal Netherlands Meteorological Institute (KNMI). Contact: (tuenter@knmi.nl). Dedicated to Prof. Dr. Nanne Weber (1959-2011).

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519 views • 39 slides

Connecting atmospheric composition with climate variability and change

Connecting atmospheric composition with climate variability and change Seminar in Atmospheric Science, EESC G9910. 9/12/12 Overview Loulergue et al., Nature, 2008 Glacial to interglacial variability (methane) Montzka et al., Nature, 2011

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458 views • 32 slides

High Latitude Insolation and Climate Response

High Latitude Insolation and Climate Response. 23 April 2009 /// EAS 4803 Sean Miller. Introduction. Milankovitch: high latitude NH summer insolation drives glacial-interglacial cycles Changes in precession (19-23 kyr cycle), obliquity (41 kyrs), eccentricity (100 kyrs) are important

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234 views • 11 slides

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METEOROLOGY

Transient (monsoonal) climate behavior in CLIMBER

Connecting atmospheric composition with climate variability and change

High Latitude Insolation and Climate Response