Response in atmospheric circulation and sources of Greenland precipitation to glacial boundary conditions

Research output: Contribution to journal › Journal article › Research › peer-review

Standard

Response in atmospheric circulation and sources of Greenland precipitation to glacial boundary conditions. / Langen, Peter Lang; Vinther, Bo Møllesøe.

In: Climate Dynamics, Vol. 32, No. 7-8, 2009, p. 1035-1054.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

Langen, PL & Vinther, BM 2009, 'Response in atmospheric circulation and sources of Greenland precipitation to glacial boundary conditions', Climate Dynamics, vol. 32, no. 7-8, pp. 1035-1054. https://doi.org/10.1007/s00382-008-0438-y

APA

Langen, P. L., & Vinther, B. M. (2009). Response in atmospheric circulation and sources of Greenland precipitation to glacial boundary conditions. Climate Dynamics, 32(7-8), 1035-1054. https://doi.org/10.1007/s00382-008-0438-y

Vancouver

Langen PL, Vinther BM. Response in atmospheric circulation and sources of Greenland precipitation to glacial boundary conditions. Climate Dynamics. 2009;32(7-8):1035-1054. https://doi.org/10.1007/s00382-008-0438-y

Author

Langen, Peter Lang ; Vinther, Bo Møllesøe. / Response in atmospheric circulation and sources of Greenland precipitation to glacial boundary conditions. In: Climate Dynamics. 2009 ; Vol. 32, No. 7-8. pp. 1035-1054.

Bibtex

@article{95988fd0117a11df803f000ea68e967b,
title = "Response in atmospheric circulation and sources of Greenland precipitation to glacial boundary conditions",
abstract = "The response in northern hemisphere atmospheric circulation and the resulting changes in moisture sources for Greenland precipitation to glacial boundary conditions are studied in NCAR's CCM3 atmospheric general circulation model fitted with a moisture tracking functionality. We employ both the CLIMAP SST reconstruction and a modification thereto with reconstructions of glacial ice sheets and land masks. The individual components of the boundary conditions are added first one at a time and, finally, together. These steps show the atmospheric circulation to respond approximately linearly to the boundary condition changes, and the full glacial change may thus be decomposed into contributions from SST and topography changes, respectively. We find that using the CLIMAP SST reconstruction leads to a shift from Atlantic toward Pacific source regions not found with the modified reconstruction having cooler tropics and less sea ice. The occurrence of such a shift depends chiefly on the SST reconstruction and not on the existence of the large northern hemisphere glacial ice sheets. The influence of these circulation changes on important factors for ice core interpretation such as precipitation seasonality, condensation temperatures and source temperatures are assessed. Udgivelsesdato: June 2009",
keywords = "Faculty of Science",
author = "Langen, {Peter Lang} and Vinther, {Bo M{\o}lles{\o}e}",
year = "2009",
doi = "10.1007/s00382-008-0438-y",
language = "English",
volume = "32",
pages = "1035--1054",
journal = "Climate Dynamics",
issn = "0930-7575",
publisher = "Springer",
number = "7-8",

}

RIS

TY - JOUR

T1 - Response in atmospheric circulation and sources of Greenland precipitation to glacial boundary conditions

AU - Langen, Peter Lang

AU - Vinther, Bo Møllesøe

PY - 2009

Y1 - 2009

N2 - The response in northern hemisphere atmospheric circulation and the resulting changes in moisture sources for Greenland precipitation to glacial boundary conditions are studied in NCAR's CCM3 atmospheric general circulation model fitted with a moisture tracking functionality. We employ both the CLIMAP SST reconstruction and a modification thereto with reconstructions of glacial ice sheets and land masks. The individual components of the boundary conditions are added first one at a time and, finally, together. These steps show the atmospheric circulation to respond approximately linearly to the boundary condition changes, and the full glacial change may thus be decomposed into contributions from SST and topography changes, respectively. We find that using the CLIMAP SST reconstruction leads to a shift from Atlantic toward Pacific source regions not found with the modified reconstruction having cooler tropics and less sea ice. The occurrence of such a shift depends chiefly on the SST reconstruction and not on the existence of the large northern hemisphere glacial ice sheets. The influence of these circulation changes on important factors for ice core interpretation such as precipitation seasonality, condensation temperatures and source temperatures are assessed. Udgivelsesdato: June 2009

AB - The response in northern hemisphere atmospheric circulation and the resulting changes in moisture sources for Greenland precipitation to glacial boundary conditions are studied in NCAR's CCM3 atmospheric general circulation model fitted with a moisture tracking functionality. We employ both the CLIMAP SST reconstruction and a modification thereto with reconstructions of glacial ice sheets and land masks. The individual components of the boundary conditions are added first one at a time and, finally, together. These steps show the atmospheric circulation to respond approximately linearly to the boundary condition changes, and the full glacial change may thus be decomposed into contributions from SST and topography changes, respectively. We find that using the CLIMAP SST reconstruction leads to a shift from Atlantic toward Pacific source regions not found with the modified reconstruction having cooler tropics and less sea ice. The occurrence of such a shift depends chiefly on the SST reconstruction and not on the existence of the large northern hemisphere glacial ice sheets. The influence of these circulation changes on important factors for ice core interpretation such as precipitation seasonality, condensation temperatures and source temperatures are assessed. Udgivelsesdato: June 2009

KW - Faculty of Science

U2 - 10.1007/s00382-008-0438-y

DO - 10.1007/s00382-008-0438-y

M3 - Journal article

VL - 32

SP - 1035

EP - 1054

JO - Climate Dynamics

JF - Climate Dynamics

SN - 0930-7575

IS - 7-8

ER -

ID: 17394350