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Greenland temperature response to climate forcing during the last deglaciation
- Source :
- Science, Science, American Association for the Advancement of Science, 2014, 345 (6201), pp.1177-1180. ⟨10.1126/SCIENCE.1254961⟩, Science, 2014, 345 (6201), pp.1177-1180. ⟨10.1126/SCIENCE.1254961⟩, Science (New York, N.Y.), vol 345, iss 6201
- Publication Year :
- 2014
- Publisher :
- HAL CCSD, 2014.
-
Abstract
- Old and older, cold and colder Greenland surface air temperatures changed dramatically during the last deglaciation. The exact amount is unknown, which makes it difficult to understand what caused those changes. Buizert et al. report temperature reconstructions for the period from 19,000 to 10,000 years before the present from three different locations in Greenland and interpret them with a climate model (see the Perspective by Sime). They provide the broad geographic pattern of temperature variability and infer the mechanisms of the changes and their seasonality, which differ in important ways from the traditional view. Science, this issue p. 1177 ; see also p. 1116
- Subjects :
- Oldest Dryas
General Science & Technology
Climate Change
Greenland
Climate change
Oxygen Isotopes
Ice core
Theoretical
Models
Freezing
Deglaciation
Computer Simulation
Ice Cover
Younger Dryas
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment
ComputingMilieux_MISCELLANEOUS
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere
Multidisciplinary
Temperature
Radiative forcing
Models, Theoretical
13. Climate action
Climatology
Abrupt climate change
Climate model
Geology
Subjects
Details
- Language :
- English
- ISSN :
- 00368075 and 10959203
- Database :
- OpenAIRE
- Journal :
- Science, Science, American Association for the Advancement of Science, 2014, 345 (6201), pp.1177-1180. ⟨10.1126/SCIENCE.1254961⟩, Science, 2014, 345 (6201), pp.1177-1180. ⟨10.1126/SCIENCE.1254961⟩, Science (New York, N.Y.), vol 345, iss 6201
- Accession number :
- edsair.doi.dedup.....16a5ae9ab02aefb3952c9eb0b2b2e9e6