Airborne measurements in a stable boundary layer over the Larsen Ice Shelf, Antarctica
We present aircraft measurements of boundary-layer structure and surface turbulent fluxes from a flight over the Larsen Ice Shelf, Antarctica. Warm advection, associated with föhn flow, led to the formation of a stable boundary layer over the ice shelf, with a well-defined low-level jet at the top o...
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Online Access: | http://nora.nerc.ac.uk/id/eprint/3218/ https://nora.nerc.ac.uk/id/eprint/3218/1/Flight_19_paper_PDFA.pdf https://doi.org/10.1007/s10546-008-9271-4 |
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ftnerc:oai:nora.nerc.ac.uk:3218 2024-06-09T07:39:39+00:00 Airborne measurements in a stable boundary layer over the Larsen Ice Shelf, Antarctica King, J.C. Lachlan-Cope, T.A. Ladkin, R.S. Weiss, A. 2008 text http://nora.nerc.ac.uk/id/eprint/3218/ https://nora.nerc.ac.uk/id/eprint/3218/1/Flight_19_paper_PDFA.pdf https://doi.org/10.1007/s10546-008-9271-4 en eng Springer https://nora.nerc.ac.uk/id/eprint/3218/1/Flight_19_paper_PDFA.pdf King, J.C. orcid:0000-0003-3315-7568 Lachlan-Cope, T.A. orcid:0000-0002-0657-3235 Ladkin, R.S.; Weiss, A. 2008 Airborne measurements in a stable boundary layer over the Larsen Ice Shelf, Antarctica. Boundary-Layer Meteorology, 127 (3). 413-428. https://doi.org/10.1007/s10546-008-9271-4 <https://doi.org/10.1007/s10546-008-9271-4> Meteorology and Climatology Glaciology Atmospheric Sciences Publication - Article PeerReviewed 2008 ftnerc https://doi.org/10.1007/s10546-008-9271-4 2024-05-15T08:44:37Z We present aircraft measurements of boundary-layer structure and surface turbulent fluxes from a flight over the Larsen Ice Shelf, Antarctica. Warm advection, associated with föhn flow, led to the formation of a stable boundary layer over the ice shelf, with a well-defined low-level jet at the top of the surface inversion. The strong shear associated with the jet kept the gradient Richardson number small and maintained a turbulent boundary layer over a depth of at least 600 m. The net surface energy balance amounted to 52 Wm−2, equivalent to a melt rate of 13 mm water per day, with net radiation (48 Wm−2) making the largest contribution to melt. The contribution from the sensible heat flux (13 Wm−2) was largely balanced by an upwards latent heat flux (−9 Wm−2). These measurements provide insight into the processes that control surface melt rates in an area that has experienced recent rapid warming and deglaciation. Article in Journal/Newspaper Antarc* Antarctica Ice Shelf Larsen Ice Shelf Natural Environment Research Council: NERC Open Research Archive Larsen Ice Shelf ENVELOPE(-62.500,-62.500,-67.500,-67.500) Boundary-Layer Meteorology 127 3 413 428 |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
English |
topic |
Meteorology and Climatology Glaciology Atmospheric Sciences |
spellingShingle |
Meteorology and Climatology Glaciology Atmospheric Sciences King, J.C. Lachlan-Cope, T.A. Ladkin, R.S. Weiss, A. Airborne measurements in a stable boundary layer over the Larsen Ice Shelf, Antarctica |
topic_facet |
Meteorology and Climatology Glaciology Atmospheric Sciences |
description |
We present aircraft measurements of boundary-layer structure and surface turbulent fluxes from a flight over the Larsen Ice Shelf, Antarctica. Warm advection, associated with föhn flow, led to the formation of a stable boundary layer over the ice shelf, with a well-defined low-level jet at the top of the surface inversion. The strong shear associated with the jet kept the gradient Richardson number small and maintained a turbulent boundary layer over a depth of at least 600 m. The net surface energy balance amounted to 52 Wm−2, equivalent to a melt rate of 13 mm water per day, with net radiation (48 Wm−2) making the largest contribution to melt. The contribution from the sensible heat flux (13 Wm−2) was largely balanced by an upwards latent heat flux (−9 Wm−2). These measurements provide insight into the processes that control surface melt rates in an area that has experienced recent rapid warming and deglaciation. |
format |
Article in Journal/Newspaper |
author |
King, J.C. Lachlan-Cope, T.A. Ladkin, R.S. Weiss, A. |
author_facet |
King, J.C. Lachlan-Cope, T.A. Ladkin, R.S. Weiss, A. |
author_sort |
King, J.C. |
title |
Airborne measurements in a stable boundary layer over the Larsen Ice Shelf, Antarctica |
title_short |
Airborne measurements in a stable boundary layer over the Larsen Ice Shelf, Antarctica |
title_full |
Airborne measurements in a stable boundary layer over the Larsen Ice Shelf, Antarctica |
title_fullStr |
Airborne measurements in a stable boundary layer over the Larsen Ice Shelf, Antarctica |
title_full_unstemmed |
Airborne measurements in a stable boundary layer over the Larsen Ice Shelf, Antarctica |
title_sort |
airborne measurements in a stable boundary layer over the larsen ice shelf, antarctica |
publisher |
Springer |
publishDate |
2008 |
url |
http://nora.nerc.ac.uk/id/eprint/3218/ https://nora.nerc.ac.uk/id/eprint/3218/1/Flight_19_paper_PDFA.pdf https://doi.org/10.1007/s10546-008-9271-4 |
long_lat |
ENVELOPE(-62.500,-62.500,-67.500,-67.500) |
geographic |
Larsen Ice Shelf |
geographic_facet |
Larsen Ice Shelf |
genre |
Antarc* Antarctica Ice Shelf Larsen Ice Shelf |
genre_facet |
Antarc* Antarctica Ice Shelf Larsen Ice Shelf |
op_relation |
https://nora.nerc.ac.uk/id/eprint/3218/1/Flight_19_paper_PDFA.pdf King, J.C. orcid:0000-0003-3315-7568 Lachlan-Cope, T.A. orcid:0000-0002-0657-3235 Ladkin, R.S.; Weiss, A. 2008 Airborne measurements in a stable boundary layer over the Larsen Ice Shelf, Antarctica. Boundary-Layer Meteorology, 127 (3). 413-428. https://doi.org/10.1007/s10546-008-9271-4 <https://doi.org/10.1007/s10546-008-9271-4> |
op_doi |
https://doi.org/10.1007/s10546-008-9271-4 |
container_title |
Boundary-Layer Meteorology |
container_volume |
127 |
container_issue |
3 |
container_start_page |
413 |
op_container_end_page |
428 |
_version_ |
1801380975475687424 |