TEMPERATURE CHANGE IS THE MAJOR DRIVER OF LATE-GLACIAL AND HOLOCENE GLACIER FLUCTUATIONS IN NEW ZEALAND

Anderson B.; Mackintosh A.

dc.contributor.author	Anderson B.
dc.contributor.author	Mackintosh A.
dc.date.accessioned	2025-01-04T06:14:11Z
dc.date.available	2025-01-04T06:14:11Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=14096493
dc.identifier.citation	Geology, 2006, 34, 2, 121-124
dc.identifier.issn	0091-7613
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/47309
dc.description.abstract	Advance and retreat of temperate glaciers is largely controlled by changes in temperature and precipitation, but the relative importance of these drivers is debated. Numerical modeling of a New Zealand glacier reveals that temperature is the dominant control on glacier length. We find that a glacial advance, dated to ca. 13,000 yr B.P., requires a cooling event of 3-4 °C. This mid-latitude Southern Hemisphere cooling is similar in magnitude to the Antarctic Cold Reversal in the Vostok ice core record and likely to be a response to the same climate signal. © 2006 Geological Society of America.
dc.subject	GLACIERS
dc.subject	LITTLE ICE AGE
dc.subject	NEW ZEALAND
dc.subject	SOUTHERN HEMISPHERE
dc.subject	YOUNGER DRYAS
dc.subject	Holocene
dc.title	TEMPERATURE CHANGE IS THE MAJOR DRIVER OF LATE-GLACIAL AND HOLOCENE GLACIER FLUCTUATIONS IN NEW ZEALAND
dc.type	Статья
dc.identifier.doi	10.1130/G22151.1
dc.subject.age	Cenozoic::Quaternary::Holocene
dc.subject.age	Кайнозой::Четвертичная::Голоцен