Atmospheric circulation over Patagonia from the Jurassic to present: A review through proxy data and climatic modelling scenarios

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This paper discusses the general atmospheric circulation over Patagonia on the basis of the principal palaeoclimate forcings: continental drift, orography, variations in the greenhouse gases in the Earth's atmosphere, evolution of the atmosphere and the oceans, changes in the orbit of the Earth...

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Autor principal:	Compagnucci, R.H.
Formato:	JOUR
Materias:	Palaeo-winds Palaeoclimate Palaeoclimate forcings Westerlies albedo atmospheric circulation climate forcing climate modeling continental drift Cretaceous greenhouse gas Hypsithermal Jurassic Last Glacial Maximum Oligocene orbital forcing orography paleoatmosphere paleoclimate Pliocene proxy climate record Tortonian Patagonia
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00244066_v103_n2_p229_Compagnucci
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	todo:paper_00244066_v103_n2_p229_Compagnucci
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spelling	todo:paper_00244066_v103_n2_p229_Compagnucci2023-10-03T14:34:51Z Atmospheric circulation over Patagonia from the Jurassic to present: A review through proxy data and climatic modelling scenarios Compagnucci, R.H. Palaeo-winds Palaeoclimate Palaeoclimate forcings Westerlies albedo atmospheric circulation climate forcing climate modeling continental drift Cretaceous greenhouse gas Hypsithermal Jurassic Last Glacial Maximum Oligocene orbital forcing orography paleoatmosphere paleoclimate Pliocene proxy climate record Tortonian Patagonia This paper discusses the general atmospheric circulation over Patagonia on the basis of the principal palaeoclimate forcings: continental drift, orography, variations in the greenhouse gases in the Earth's atmosphere, evolution of the atmosphere and the oceans, changes in the orbit of the Earth, albedo feedbacks, and the land surface. These processes affect climate on time scales of millions to hundreds of thousands of years. Additionally, orbital forcing has had a major influence on climate during the Quaternary. The palaeo-atmospheric circulation of Patagonia is analyzed for the Early to Late Jurassic, the Cretaceous, the Late Palaeocene-Eocene Thermal Maximum, the Tortonian-Oligocene cooling, the Pliocene, the Quaternary including the Last Glacial Maximum, the Holocene Optimum, and the last millennium changes. Alternative palaeo-atmospheric circulations from climatic modelling scenarios through the ages are reviewed and compared with proxy data. Detailed and updated reference information on the topics analyzed is also provided. © 2011 The Linnean Society of London. Fil:Compagnucci, R.H. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00244066_v103_n2_p229_Compagnucci
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Palaeo-winds Palaeoclimate Palaeoclimate forcings Westerlies albedo atmospheric circulation climate forcing climate modeling continental drift Cretaceous greenhouse gas Hypsithermal Jurassic Last Glacial Maximum Oligocene orbital forcing orography paleoatmosphere paleoclimate Pliocene proxy climate record Tortonian Patagonia
spellingShingle	Palaeo-winds Palaeoclimate Palaeoclimate forcings Westerlies albedo atmospheric circulation climate forcing climate modeling continental drift Cretaceous greenhouse gas Hypsithermal Jurassic Last Glacial Maximum Oligocene orbital forcing orography paleoatmosphere paleoclimate Pliocene proxy climate record Tortonian Patagonia Compagnucci, R.H. Atmospheric circulation over Patagonia from the Jurassic to present: A review through proxy data and climatic modelling scenarios
topic_facet	Palaeo-winds Palaeoclimate Palaeoclimate forcings Westerlies albedo atmospheric circulation climate forcing climate modeling continental drift Cretaceous greenhouse gas Hypsithermal Jurassic Last Glacial Maximum Oligocene orbital forcing orography paleoatmosphere paleoclimate Pliocene proxy climate record Tortonian Patagonia
description	This paper discusses the general atmospheric circulation over Patagonia on the basis of the principal palaeoclimate forcings: continental drift, orography, variations in the greenhouse gases in the Earth's atmosphere, evolution of the atmosphere and the oceans, changes in the orbit of the Earth, albedo feedbacks, and the land surface. These processes affect climate on time scales of millions to hundreds of thousands of years. Additionally, orbital forcing has had a major influence on climate during the Quaternary. The palaeo-atmospheric circulation of Patagonia is analyzed for the Early to Late Jurassic, the Cretaceous, the Late Palaeocene-Eocene Thermal Maximum, the Tortonian-Oligocene cooling, the Pliocene, the Quaternary including the Last Glacial Maximum, the Holocene Optimum, and the last millennium changes. Alternative palaeo-atmospheric circulations from climatic modelling scenarios through the ages are reviewed and compared with proxy data. Detailed and updated reference information on the topics analyzed is also provided. © 2011 The Linnean Society of London.
format	JOUR
author	Compagnucci, R.H.
author_facet	Compagnucci, R.H.
author_sort	Compagnucci, R.H.
title	Atmospheric circulation over Patagonia from the Jurassic to present: A review through proxy data and climatic modelling scenarios
title_short	Atmospheric circulation over Patagonia from the Jurassic to present: A review through proxy data and climatic modelling scenarios
title_full	Atmospheric circulation over Patagonia from the Jurassic to present: A review through proxy data and climatic modelling scenarios
title_fullStr	Atmospheric circulation over Patagonia from the Jurassic to present: A review through proxy data and climatic modelling scenarios
title_full_unstemmed	Atmospheric circulation over Patagonia from the Jurassic to present: A review through proxy data and climatic modelling scenarios
title_sort	atmospheric circulation over patagonia from the jurassic to present: a review through proxy data and climatic modelling scenarios
url	http://hdl.handle.net/20.500.12110/paper_00244066_v103_n2_p229_Compagnucci
work_keys_str_mv	AT compagnuccirh atmosphericcirculationoverpatagoniafromthejurassictopresentareviewthroughproxydataandclimaticmodellingscenarios
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Atmospheric circulation over Patagonia from the Jurassic to present: A review through proxy data and climatic modelling scenarios

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