Abstract
| Originalsprog | Engelsk |
|---|---|
| Tidsskrift | Journal of Geophysical Research - Atmospheres |
| Vol/bind | 111 |
| Udgave nummer | D15 |
| Sider (fra-til) | D15106 |
| ISSN | 0196-2256 |
| DOI | |
| Status | Udgivet - 2006 |
Bibliografisk note
Paper id:: doi:10.1029/2005JD006765Adgang til dokumentet
- 2005JD006765 preprintIndsendt manuskript, 453 KB
- 2005JD006765Forlagets udgivne version, 586 KB
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Retrieving a common accumulation record from Greenland ice cores for the past 1800 years. / Andersen, Katrine K.; Ditlevsen, Peter D.; Rasmussen, Sune Olander; Clausen, Henrik Brink; Vinther, Bo Møllesøe; Johnsen, Sigfus Johann; Steffensen, Jørgen Peder.
I: Journal of Geophysical Research - Atmospheres, Bind 111, Nr. D15, 2006, s. D15106.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › peer review
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TY - JOUR
T1 - Retrieving a common accumulation record from Greenland ice cores for the past 1800 years
AU - Andersen, Katrine K.
AU - Ditlevsen, Peter D.
AU - Rasmussen, Sune Olander
AU - Clausen, Henrik Brink
AU - Vinther, Bo Møllesøe
AU - Johnsen, Sigfus Johann
AU - Steffensen, Jørgen Peder
N1 - Paper id:: doi:10.1029/2005JD006765
PY - 2006
Y1 - 2006
N2 - In the accumulation zone of the Greenland ice sheet the annual accumulation rate may be determined through identification of the annual cycle in the isotopic climate signal and other parameters that exhibit seasonal variations. On an annual basis the accumulation rate in different Greenland ice cores is highly variable, and the degree of correlation between accumulation series from different ice cores is low. However, when using multiyear averages of the different accumulation records, the correlation increases significantly. A statistical model has been developed to estimate the common climate signal in the different accumulation records through optimization of the ratio between the variance of the common signal and of the residual. Using this model, a common Greenland accumulation record for the past 1800 years has been extracted. The record shows significant 11.9 years periodicity. A sharp transition to very dry conditions is found just before A.D. 1200, and very dry conditions during the 13th century together with dry and cold spells during the 14th century may have put extra strain on the Norse population in Greenland and may have contributed to their extinction. Accumulation rates gradually decrease from a distinct maximum in A.D. 1394 to very dry conditions in the late 17th century and thus reflect the Little Ice Age.
AB - In the accumulation zone of the Greenland ice sheet the annual accumulation rate may be determined through identification of the annual cycle in the isotopic climate signal and other parameters that exhibit seasonal variations. On an annual basis the accumulation rate in different Greenland ice cores is highly variable, and the degree of correlation between accumulation series from different ice cores is low. However, when using multiyear averages of the different accumulation records, the correlation increases significantly. A statistical model has been developed to estimate the common climate signal in the different accumulation records through optimization of the ratio between the variance of the common signal and of the residual. Using this model, a common Greenland accumulation record for the past 1800 years has been extracted. The record shows significant 11.9 years periodicity. A sharp transition to very dry conditions is found just before A.D. 1200, and very dry conditions during the 13th century together with dry and cold spells during the 14th century may have put extra strain on the Norse population in Greenland and may have contributed to their extinction. Accumulation rates gradually decrease from a distinct maximum in A.D. 1394 to very dry conditions in the late 17th century and thus reflect the Little Ice Age.
U2 - 10.1029/2005JD006765
DO - 10.1029/2005JD006765
M3 - Journal article
VL - 111
SP - D15106
JO - Journal of Geophysical Research: Solid Earth
JF - Journal of Geophysical Research: Solid Earth
SN - 0148-0227
IS - D15
ER -