How to combine sparse proxy data and coupled climate models

Author:

Paul André,Schäfer-Neth Christian

Publisher

Elsevier BV

Subject

Geology,Archaeology,Archaeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference37 articles.

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2. CLIMAP Project Members, 1981. Seasonal reconstructions of the Earth's surface at the last glacial maximum. Geological Society of America, Map and Chart Series MC-36, 1–18.

3. CLIMAP SSTs re-revisited;Crowley;Climate Dynamics,2000

4. An atmospheric energy–moisture balance model;Fanning;Journal of Geophysical Research,1996

5. Gersonde, R., Abelmann, A., Brathauer, U., Cortese, G., Fütterer, D., Grobe, H., Niebler, H.-S., Segl, M., Sieger, R., Zielinski, U., 2003. Last glacial maximum sea surface temperature and sea ice extent in the Southern Ocean (Atlantic-Indian sector). a multiproxy approach. Paleoceanography 18, doi 10.1029/2002PA00773.

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