Phased Patagonian Ice Sheet response to Southern Hemisphere atmospheric and oceanic warming between 18 and 17 ka

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Location: Deutsche Nationalbibliothek Frankfurt am Main

ISSN: 2045-2322

Extent: Online-Ressource

Language: Englisch

Notes: online resource.

Bibliographic citation: Phased Patagonian Ice Sheet response to Southern Hemisphere atmospheric and oceanic warming between 18 and 17 ka ; volume:9 ; number:1 ; day:11 ; month:3 ; year:2019 ; pages:1-9 ; date:12.2019
Scientific reports ; 9, Heft 1 (11.3.2019), 1-9, 12.2019

Classification: Naturwissenschaften

Creator: Bendle, Jacob M.
Palmer, Adrian P.
Thorndycraft, Varyl R.
Matthews, Ian P.

Contributor: SpringerLink (Online service)

DOI: 10.1038/s41598-019-39750-w

URN: urn:nbn:de:101:1-2019033100061503147318

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 14.08.2025, 10:51 AM CEST

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Bendle, Jacob M.
Palmer, Adrian P.
Thorndycraft, Varyl R.
Matthews, Ian P.
SpringerLink (Online service)

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Attributing observed permafrost warming in the northern hemisphere to anthropogenic climate change

Southern Hemisphere anticyclonic circulation drives oceanic and climatic conditions in late Holocene southernmost Africa

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Oceanic primary production decline halved in eddy-resolving simulations of global warming

Maximum Northern Hemisphere warming rates before and after 1880 during the Common Era

Southern-Hemisphere high-latitude stratospheric warming revisit

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The dynamics of the warming hiatus over the Northern Hemisphere

Earlier ice loss accelerates lake warming in the Northern Hemisphere

A cleaner snow future mitigates Northern Hemisphere snowpack loss from warming

Anomalous Arctic warming linked with severe winter weather in Northern Hemisphere continents

Attributing observed permafrost warming in the northern hemisphere to anthropogenic climate change

Southern Hemisphere anticyclonic circulation drives oceanic and climatic conditions in late Holocene southernmost Africa

Abschnitt

Table II. - Fuegian and Patagonian.

Oceanic primary production decline halved in eddy-resolving simulations of global warming

Maximum Northern Hemisphere warming rates before and after 1880 during the Common Era

Southern-Hemisphere high-latitude stratospheric warming revisit

Stratospheric warming in Southern Hemisphere high latitudes since 1979

The dynamics of the warming hiatus over the Northern Hemisphere

Earlier ice loss accelerates lake warming in the Northern Hemisphere

A cleaner snow future mitigates Northern Hemisphere snowpack loss from warming

Anomalous Arctic warming linked with severe winter weather in Northern Hemisphere continents

Attributing observed permafrost warming in the northern hemisphere to anthropogenic climate change

Southern Hemisphere anticyclonic circulation drives oceanic and climatic conditions in late Holocene southernmost Africa

Abschnitt

Table II. - Fuegian and Patagonian.

Oceanic primary production decline halved in eddy-resolving simulations of global warming

Maximum Northern Hemisphere warming rates before and after 1880 during the Common Era

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Phased Patagonian Ice Sheet response to Southern Hemisphere atmospheric and oceanic warming between 18 and 17 ka

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Other Objects (12)

Southern-Hemisphere high-latitude stratospheric warming revisit

Stratospheric warming in Southern Hemisphere high latitudes since 1979

The dynamics of the warming hiatus over the Northern Hemisphere

Earlier ice loss accelerates lake warming in the Northern Hemisphere

A cleaner snow future mitigates Northern Hemisphere snowpack loss from warming

Anomalous Arctic warming linked with severe winter weather in Northern Hemisphere continents

Attributing observed permafrost warming in the northern hemisphere to anthropogenic climate change

Southern Hemisphere anticyclonic circulation drives oceanic and climatic conditions in late Holocene southernmost Africa

Table II. - Fuegian and Patagonian.

Oceanic primary production decline halved in eddy-resolving simulations of global warming

Oceanic primary production decline halved in eddy-resolving simulations of global warming

Maximum Northern Hemisphere warming rates before and after 1880 during the Common Era

Southern-Hemisphere high-latitude stratospheric warming revisit

Stratospheric warming in Southern Hemisphere high latitudes since 1979

The dynamics of the warming hiatus over the Northern Hemisphere

Earlier ice loss accelerates lake warming in the Northern Hemisphere

A cleaner snow future mitigates Northern Hemisphere snowpack loss from warming

Anomalous Arctic warming linked with severe winter weather in Northern Hemisphere continents

Attributing observed permafrost warming in the northern hemisphere to anthropogenic climate change

Southern Hemisphere anticyclonic circulation drives oceanic and climatic conditions in late Holocene southernmost Africa

Table II. - Fuegian and Patagonian.

Oceanic primary production decline halved in eddy-resolving simulations of global warming

Oceanic primary production decline halved in eddy-resolving simulations of global warming

Maximum Northern Hemisphere warming rates before and after 1880 during the Common Era

Southern-Hemisphere high-latitude stratospheric warming revisit

Stratospheric warming in Southern Hemisphere high latitudes since 1979

The dynamics of the warming hiatus over the Northern Hemisphere

Earlier ice loss accelerates lake warming in the Northern Hemisphere

A cleaner snow future mitigates Northern Hemisphere snowpack loss from warming

Anomalous Arctic warming linked with severe winter weather in Northern Hemisphere continents

Attributing observed permafrost warming in the northern hemisphere to anthropogenic climate change

Southern Hemisphere anticyclonic circulation drives oceanic and climatic conditions in late Holocene southernmost Africa

Table II. - Fuegian and Patagonian.

Oceanic primary production decline halved in eddy-resolving simulations of global warming

Oceanic primary production decline halved in eddy-resolving simulations of global warming

Maximum Northern Hemisphere warming rates before and after 1880 during the Common Era

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