Modeling the water isotopes in Greenland precipitation 1959–2001 with the meso-scale model REMO-iso
Ice core studies have proved thed18O in Greenland precipitation to be correlated to thephase of the North Atlantic Oscillation (NAO). This subject has also been investigated inmodeling studies. However, these studies have either had severe biases in thed18O levels,or have not been designed to be com...
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ftulundlup:oai:lup.lub.lu.se:b7379750-d336-4ef0-9fb1-897afe8c45b6 2023-05-15T16:23:48+02:00 Modeling the water isotopes in Greenland precipitation 1959–2001 with the meso-scale model REMO-iso Sjolte, J. Hoffmann, G. Johnsen, S. J. Vinther, B. M. Masson-delmotte, V. Sturm, C. 2011 https://lup.lub.lu.se/record/b7379750-d336-4ef0-9fb1-897afe8c45b6 https://doi.org/10.1029/2010JD015287 eng eng Wiley-Blackwell https://lup.lub.lu.se/record/b7379750-d336-4ef0-9fb1-897afe8c45b6 http://dx.doi.org/10.1029/2010JD015287 scopus:80053363455 Journal of Geophysical Research; 116(D18), pp 1-22 (2011) ISSN: 0148-0227 Meteorology and Atmospheric Sciences contributiontojournal/article info:eu-repo/semantics/article text 2011 ftulundlup https://doi.org/10.1029/2010JD015287 2023-02-01T23:37:23Z Ice core studies have proved thed18O in Greenland precipitation to be correlated to thephase of the North Atlantic Oscillation (NAO). This subject has also been investigated inmodeling studies. However, these studies have either had severe biases in thed18O levels,or have not been designed to be compared directly with observations. In this study wenudge a meso‐scale climate model fitted with stable water isotope diagnostics (REMO‐iso)to follow the actual weather patterns for the period 1959–2001. We evaluate thissimulation using meteorological observations from stations along the Greenland coast,andd18O from several Greenland ice core stacks and Global Network In Precipitation(GNIP) data from Greenland, Iceland and Svalbard. The REMO‐iso output explains up to40% of the interannuald18O variability observed in ice cores, which is comparable to themodel performance for precipitation. In terms of reproducing the observed variabilitythe global model, ECHAM4‐iso performs on the same level as REMO‐iso. However,REMO‐iso has smaller biases ind18O and improved representation of the observed spatiald18O‐temperature slope compared to ECHAM4‐iso. Analysis of the main modes of wintervariability ofd18O shows a coherent signal in Central and Western Greenland similarto results from ice cores. The NAO explains 20% of the leadingd18O pattern. Based on themodel output we suggest that methods to reconstruct the NAO from Greenland ice coresemploy bothd18O and accumulation records Article in Journal/Newspaper Greenland Greenland ice core ice core Iceland North Atlantic North Atlantic oscillation Svalbard Lund University Publications (LUP) Greenland Remo ENVELOPE(-128.718,-128.718,54.496,54.496) Svalbard Journal of Geophysical Research 116 D18 |
institution |
Open Polar |
collection |
Lund University Publications (LUP) |
op_collection_id |
ftulundlup |
language |
English |
topic |
Meteorology and Atmospheric Sciences |
spellingShingle |
Meteorology and Atmospheric Sciences Sjolte, J. Hoffmann, G. Johnsen, S. J. Vinther, B. M. Masson-delmotte, V. Sturm, C. Modeling the water isotopes in Greenland precipitation 1959–2001 with the meso-scale model REMO-iso |
topic_facet |
Meteorology and Atmospheric Sciences |
description |
Ice core studies have proved thed18O in Greenland precipitation to be correlated to thephase of the North Atlantic Oscillation (NAO). This subject has also been investigated inmodeling studies. However, these studies have either had severe biases in thed18O levels,or have not been designed to be compared directly with observations. In this study wenudge a meso‐scale climate model fitted with stable water isotope diagnostics (REMO‐iso)to follow the actual weather patterns for the period 1959–2001. We evaluate thissimulation using meteorological observations from stations along the Greenland coast,andd18O from several Greenland ice core stacks and Global Network In Precipitation(GNIP) data from Greenland, Iceland and Svalbard. The REMO‐iso output explains up to40% of the interannuald18O variability observed in ice cores, which is comparable to themodel performance for precipitation. In terms of reproducing the observed variabilitythe global model, ECHAM4‐iso performs on the same level as REMO‐iso. However,REMO‐iso has smaller biases ind18O and improved representation of the observed spatiald18O‐temperature slope compared to ECHAM4‐iso. Analysis of the main modes of wintervariability ofd18O shows a coherent signal in Central and Western Greenland similarto results from ice cores. The NAO explains 20% of the leadingd18O pattern. Based on themodel output we suggest that methods to reconstruct the NAO from Greenland ice coresemploy bothd18O and accumulation records |
format |
Article in Journal/Newspaper |
author |
Sjolte, J. Hoffmann, G. Johnsen, S. J. Vinther, B. M. Masson-delmotte, V. Sturm, C. |
author_facet |
Sjolte, J. Hoffmann, G. Johnsen, S. J. Vinther, B. M. Masson-delmotte, V. Sturm, C. |
author_sort |
Sjolte, J. |
title |
Modeling the water isotopes in Greenland precipitation 1959–2001 with the meso-scale model REMO-iso |
title_short |
Modeling the water isotopes in Greenland precipitation 1959–2001 with the meso-scale model REMO-iso |
title_full |
Modeling the water isotopes in Greenland precipitation 1959–2001 with the meso-scale model REMO-iso |
title_fullStr |
Modeling the water isotopes in Greenland precipitation 1959–2001 with the meso-scale model REMO-iso |
title_full_unstemmed |
Modeling the water isotopes in Greenland precipitation 1959–2001 with the meso-scale model REMO-iso |
title_sort |
modeling the water isotopes in greenland precipitation 1959–2001 with the meso-scale model remo-iso |
publisher |
Wiley-Blackwell |
publishDate |
2011 |
url |
https://lup.lub.lu.se/record/b7379750-d336-4ef0-9fb1-897afe8c45b6 https://doi.org/10.1029/2010JD015287 |
long_lat |
ENVELOPE(-128.718,-128.718,54.496,54.496) |
geographic |
Greenland Remo Svalbard |
geographic_facet |
Greenland Remo Svalbard |
genre |
Greenland Greenland ice core ice core Iceland North Atlantic North Atlantic oscillation Svalbard |
genre_facet |
Greenland Greenland ice core ice core Iceland North Atlantic North Atlantic oscillation Svalbard |
op_source |
Journal of Geophysical Research; 116(D18), pp 1-22 (2011) ISSN: 0148-0227 |
op_relation |
https://lup.lub.lu.se/record/b7379750-d336-4ef0-9fb1-897afe8c45b6 http://dx.doi.org/10.1029/2010JD015287 scopus:80053363455 |
op_doi |
https://doi.org/10.1029/2010JD015287 |
container_title |
Journal of Geophysical Research |
container_volume |
116 |
container_issue |
D18 |
_version_ |
1766012115532906496 |