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Regional Antarctic snow accumulation over the past 1000 years
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| Zeitschriftentitel: | Climate of the Past |
|---|---|
| Personen und Körperschaften: | , , , , , , , , , , , , , , , |
| In: | Climate of the Past, 13, 2017, 11, S. 1491-1513 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
Copernicus GmbH
|
| Schlagwörter: |
| author_facet |
Thomas, Elizabeth R. van Wessem, J. Melchior Roberts, Jason Isaksson, Elisabeth Schlosser, Elisabeth Fudge, Tyler J. Vallelonga, Paul Medley, Brooke Lenaerts, Jan Bertler, Nancy van den Broeke, Michiel R. Dixon, Daniel A. Frezzotti, Massimo Stenni, Barbara Curran, Mark Ekaykin, Alexey A. Thomas, Elizabeth R. van Wessem, J. Melchior Roberts, Jason Isaksson, Elisabeth Schlosser, Elisabeth Fudge, Tyler J. Vallelonga, Paul Medley, Brooke Lenaerts, Jan Bertler, Nancy van den Broeke, Michiel R. Dixon, Daniel A. Frezzotti, Massimo Stenni, Barbara Curran, Mark Ekaykin, Alexey A. |
|---|---|
| author |
Thomas, Elizabeth R. van Wessem, J. Melchior Roberts, Jason Isaksson, Elisabeth Schlosser, Elisabeth Fudge, Tyler J. Vallelonga, Paul Medley, Brooke Lenaerts, Jan Bertler, Nancy van den Broeke, Michiel R. Dixon, Daniel A. Frezzotti, Massimo Stenni, Barbara Curran, Mark Ekaykin, Alexey A. |
| spellingShingle |
Thomas, Elizabeth R. van Wessem, J. Melchior Roberts, Jason Isaksson, Elisabeth Schlosser, Elisabeth Fudge, Tyler J. Vallelonga, Paul Medley, Brooke Lenaerts, Jan Bertler, Nancy van den Broeke, Michiel R. Dixon, Daniel A. Frezzotti, Massimo Stenni, Barbara Curran, Mark Ekaykin, Alexey A. Climate of the Past Regional Antarctic snow accumulation over the past 1000 years Paleontology Stratigraphy Global and Planetary Change |
| author_sort |
thomas, elizabeth r. |
| spelling |
Thomas, Elizabeth R. van Wessem, J. Melchior Roberts, Jason Isaksson, Elisabeth Schlosser, Elisabeth Fudge, Tyler J. Vallelonga, Paul Medley, Brooke Lenaerts, Jan Bertler, Nancy van den Broeke, Michiel R. Dixon, Daniel A. Frezzotti, Massimo Stenni, Barbara Curran, Mark Ekaykin, Alexey A. 1814-9332 Copernicus GmbH Paleontology Stratigraphy Global and Planetary Change http://dx.doi.org/10.5194/cp-13-1491-2017 <jats:p>Abstract. Here we present Antarctic snow accumulation variability at the regional scale over the past 1000 years. A total of 79 ice core snow accumulation records were gathered and assigned to seven geographical regions, separating the high-accumulation coastal zones below 2000 m of elevation from the dry central Antarctic Plateau. The regional composites of annual snow accumulation were evaluated against modelled surface mass balance (SMB) from RACMO2.3p2 and precipitation from ERA-Interim reanalysis. With the exception of the Weddell Sea coast, the low-elevation composites capture the regional precipitation and SMB variability as defined by the models. The central Antarctic sites lack coherency and either do not represent regional precipitation or indicate the model inability to capture relevant precipitation processes in the cold, dry central plateau. Our results show that SMB for the total Antarctic Ice Sheet (including ice shelves) has increased at a rate of 7 ± 0.13 Gt decade−1 since 1800 AD, representing a net reduction in sea level of ∼ 0.02 mm decade−1 since 1800 and ∼ 0.04 mm decade−1 since 1900 AD. The largest contribution is from the Antarctic Peninsula (∼ 75 %) where the annual average SMB during the most recent decade (2001–2010) is 123 ± 44 Gt yr−1 higher than the annual average during the first decade of the 19th century. Only four ice core records cover the full 1000 years, and they suggest a decrease in snow accumulation during this period. However, our study emphasizes the importance of low-elevation coastal zones, which have been under-represented in previous investigations of temporal snow accumulation. </jats:p> Regional Antarctic snow accumulation over the past 1000 years Climate of the Past |
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| title |
Regional Antarctic snow accumulation over the past 1000 years |
| title_unstemmed |
Regional Antarctic snow accumulation over the past 1000 years |
| title_full |
Regional Antarctic snow accumulation over the past 1000 years |
| title_fullStr |
Regional Antarctic snow accumulation over the past 1000 years |
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Regional Antarctic snow accumulation over the past 1000 years |
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Regional Antarctic snow accumulation over the past 1000 years |
| title_sort |
regional antarctic snow accumulation over the past 1000 years |
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Paleontology Stratigraphy Global and Planetary Change |
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http://dx.doi.org/10.5194/cp-13-1491-2017 |
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2017 |
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1491-1513 |
| description |
<jats:p>Abstract. Here we present Antarctic snow accumulation variability at the regional scale over the past 1000 years. A total of 79 ice core snow accumulation records were gathered and assigned to seven geographical regions, separating the high-accumulation coastal zones below 2000 m of elevation from the dry central Antarctic Plateau. The regional composites of annual snow accumulation were evaluated against modelled surface mass balance (SMB) from RACMO2.3p2 and precipitation from ERA-Interim reanalysis. With the exception of the Weddell Sea coast, the low-elevation composites capture the regional precipitation and SMB variability as defined by the models. The central Antarctic sites lack coherency and either do not represent regional precipitation or indicate the model inability to capture relevant precipitation processes in the cold, dry central plateau. Our results show that SMB for the total Antarctic Ice Sheet (including ice shelves) has increased at a rate of 7 ± 0.13 Gt decade−1 since 1800 AD, representing a net reduction in sea level of ∼ 0.02 mm decade−1 since 1800 and ∼ 0.04 mm decade−1 since 1900 AD. The largest contribution is from the Antarctic Peninsula (∼ 75 %) where the annual average SMB during the most recent decade (2001–2010) is 123 ± 44 Gt yr−1 higher than the annual average during the first decade of the 19th century. Only four ice core records cover the full 1000 years, and they suggest a decrease in snow accumulation during this period. However, our study emphasizes the importance of low-elevation coastal zones, which have been under-represented in previous investigations of temporal snow accumulation.
</jats:p> |
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| author | Thomas, Elizabeth R., van Wessem, J. Melchior, Roberts, Jason, Isaksson, Elisabeth, Schlosser, Elisabeth, Fudge, Tyler J., Vallelonga, Paul, Medley, Brooke, Lenaerts, Jan, Bertler, Nancy, van den Broeke, Michiel R., Dixon, Daniel A., Frezzotti, Massimo, Stenni, Barbara, Curran, Mark, Ekaykin, Alexey A. |
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| description | <jats:p>Abstract. Here we present Antarctic snow accumulation variability at the regional scale over the past 1000 years. A total of 79 ice core snow accumulation records were gathered and assigned to seven geographical regions, separating the high-accumulation coastal zones below 2000 m of elevation from the dry central Antarctic Plateau. The regional composites of annual snow accumulation were evaluated against modelled surface mass balance (SMB) from RACMO2.3p2 and precipitation from ERA-Interim reanalysis. With the exception of the Weddell Sea coast, the low-elevation composites capture the regional precipitation and SMB variability as defined by the models. The central Antarctic sites lack coherency and either do not represent regional precipitation or indicate the model inability to capture relevant precipitation processes in the cold, dry central plateau. Our results show that SMB for the total Antarctic Ice Sheet (including ice shelves) has increased at a rate of 7 ± 0.13 Gt decade−1 since 1800 AD, representing a net reduction in sea level of ∼ 0.02 mm decade−1 since 1800 and ∼ 0.04 mm decade−1 since 1900 AD. The largest contribution is from the Antarctic Peninsula (∼ 75 %) where the annual average SMB during the most recent decade (2001–2010) is 123 ± 44 Gt yr−1 higher than the annual average during the first decade of the 19th century. Only four ice core records cover the full 1000 years, and they suggest a decrease in snow accumulation during this period. However, our study emphasizes the importance of low-elevation coastal zones, which have been under-represented in previous investigations of temporal snow accumulation. </jats:p> |
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| spelling | Thomas, Elizabeth R. van Wessem, J. Melchior Roberts, Jason Isaksson, Elisabeth Schlosser, Elisabeth Fudge, Tyler J. Vallelonga, Paul Medley, Brooke Lenaerts, Jan Bertler, Nancy van den Broeke, Michiel R. Dixon, Daniel A. Frezzotti, Massimo Stenni, Barbara Curran, Mark Ekaykin, Alexey A. 1814-9332 Copernicus GmbH Paleontology Stratigraphy Global and Planetary Change http://dx.doi.org/10.5194/cp-13-1491-2017 <jats:p>Abstract. Here we present Antarctic snow accumulation variability at the regional scale over the past 1000 years. A total of 79 ice core snow accumulation records were gathered and assigned to seven geographical regions, separating the high-accumulation coastal zones below 2000 m of elevation from the dry central Antarctic Plateau. The regional composites of annual snow accumulation were evaluated against modelled surface mass balance (SMB) from RACMO2.3p2 and precipitation from ERA-Interim reanalysis. With the exception of the Weddell Sea coast, the low-elevation composites capture the regional precipitation and SMB variability as defined by the models. The central Antarctic sites lack coherency and either do not represent regional precipitation or indicate the model inability to capture relevant precipitation processes in the cold, dry central plateau. Our results show that SMB for the total Antarctic Ice Sheet (including ice shelves) has increased at a rate of 7 ± 0.13 Gt decade−1 since 1800 AD, representing a net reduction in sea level of ∼ 0.02 mm decade−1 since 1800 and ∼ 0.04 mm decade−1 since 1900 AD. The largest contribution is from the Antarctic Peninsula (∼ 75 %) where the annual average SMB during the most recent decade (2001–2010) is 123 ± 44 Gt yr−1 higher than the annual average during the first decade of the 19th century. Only four ice core records cover the full 1000 years, and they suggest a decrease in snow accumulation during this period. However, our study emphasizes the importance of low-elevation coastal zones, which have been under-represented in previous investigations of temporal snow accumulation. </jats:p> Regional Antarctic snow accumulation over the past 1000 years Climate of the Past |
| spellingShingle | Thomas, Elizabeth R., van Wessem, J. Melchior, Roberts, Jason, Isaksson, Elisabeth, Schlosser, Elisabeth, Fudge, Tyler J., Vallelonga, Paul, Medley, Brooke, Lenaerts, Jan, Bertler, Nancy, van den Broeke, Michiel R., Dixon, Daniel A., Frezzotti, Massimo, Stenni, Barbara, Curran, Mark, Ekaykin, Alexey A., Climate of the Past, Regional Antarctic snow accumulation over the past 1000 years, Paleontology, Stratigraphy, Global and Planetary Change |
| title | Regional Antarctic snow accumulation over the past 1000 years |
| title_full | Regional Antarctic snow accumulation over the past 1000 years |
| title_fullStr | Regional Antarctic snow accumulation over the past 1000 years |
| title_full_unstemmed | Regional Antarctic snow accumulation over the past 1000 years |
| title_short | Regional Antarctic snow accumulation over the past 1000 years |
| title_sort | regional antarctic snow accumulation over the past 1000 years |
| title_unstemmed | Regional Antarctic snow accumulation over the past 1000 years |
| topic | Paleontology, Stratigraphy, Global and Planetary Change |
| url | http://dx.doi.org/10.5194/cp-13-1491-2017 |