Eintrag weiter verarbeiten
Studies of the grounding-line location on Ice Streams D and E, Antarctica
Gespeichert in:
| Zeitschriftentitel: | Annals of Glaciology |
|---|---|
| Personen und Körperschaften: | , , |
| In: | Annals of Glaciology, 20, 1994, S. 39-42 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
International Glaciological Society
|
| Schlagwörter: |
| author_facet |
Jacobel, Robert W. Robinson, Audrey E. Bindschadler, Robert A. Jacobel, Robert W. Robinson, Audrey E. Bindschadler, Robert A. |
|---|---|
| author |
Jacobel, Robert W. Robinson, Audrey E. Bindschadler, Robert A. |
| spellingShingle |
Jacobel, Robert W. Robinson, Audrey E. Bindschadler, Robert A. Annals of Glaciology Studies of the grounding-line location on Ice Streams D and E, Antarctica Earth-Surface Processes |
| author_sort |
jacobel, robert w. |
| spelling |
Jacobel, Robert W. Robinson, Audrey E. Bindschadler, Robert A. 0260-3055 1727-5644 International Glaciological Society Earth-Surface Processes http://dx.doi.org/10.3189/1994aog20-1-39-42 <jats:p>Landsat Thematic Mapper (TM) images were used prior to the 1991–92 field season to infer the position of the grounding line at the mouths of Ice Streams D and E, West Antarctica. Our field plan for mass-balance studies was based on this determination, and thus the imagery played a central role in both the scientific and logistics planning. A radar profile along the flow direction was made across the inferred grounding line at one location, and ice-thickness measurements together with surface surveying enable us to compare the hydrostatic surface and the actual topography to determine the point at which the ice becomes grounded. The profile transits from floating to grounded ice at the same location as the grounding line inferred from the imagery. Changes in the radar-echo strength also occur at this location, giving further support to this interpretation. Tilt studies of the ice flexure caused by tidal variations at locations on either side of this grounding point give additional evidence that grounding is occurring close by. The combination of these three measurements therefore confirms the grounding-line location derived from the satellite imagery and supports the use of this technique to determine grounding.</jats:p> Studies of the grounding-line location on Ice Streams D and E, Antarctica Annals of Glaciology |
| doi_str_mv |
10.3189/1994aog20-1-39-42 |
| facet_avail |
Online Free |
| finc_class_facet |
Geologie und Paläontologie Geographie |
| format |
ElectronicArticle |
| fullrecord |
blob:ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMzE4OS8xOTk0YW9nMjAtMS0zOS00Mg |
| id |
ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMzE4OS8xOTk0YW9nMjAtMS0zOS00Mg |
| institution |
DE-Gla1 DE-Zi4 DE-15 DE-Rs1 DE-Pl11 DE-105 DE-14 DE-Ch1 DE-L229 DE-D275 DE-Bn3 DE-Brt1 DE-Zwi2 DE-D161 |
| imprint |
International Glaciological Society, 1994 |
| imprint_str_mv |
International Glaciological Society, 1994 |
| issn |
0260-3055 1727-5644 |
| issn_str_mv |
0260-3055 1727-5644 |
| language |
English |
| mega_collection |
International Glaciological Society (CrossRef) |
| match_str |
jacobel1994studiesofthegroundinglinelocationonicestreamsdandeantarctica |
| publishDateSort |
1994 |
| publisher |
International Glaciological Society |
| recordtype |
ai |
| record_format |
ai |
| series |
Annals of Glaciology |
| source_id |
49 |
| title |
Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_unstemmed |
Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_full |
Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_fullStr |
Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_full_unstemmed |
Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_short |
Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_sort |
studies of the grounding-line location on ice streams d and e, antarctica |
| topic |
Earth-Surface Processes |
| url |
http://dx.doi.org/10.3189/1994aog20-1-39-42 |
| publishDate |
1994 |
| physical |
39-42 |
| description |
<jats:p>Landsat Thematic Mapper (TM) images were used prior to the 1991–92 field season to infer the position of the grounding line at the mouths of Ice Streams D and E, West Antarctica. Our field plan for mass-balance studies was based on this determination, and thus the imagery played a central role in both the scientific and logistics planning. A radar profile along the flow direction was made across the inferred grounding line at one location, and ice-thickness measurements together with surface surveying enable us to compare the hydrostatic surface and the actual topography to determine the point at which the ice becomes grounded. The profile transits from floating to grounded ice at the same location as the grounding line inferred from the imagery. Changes in the radar-echo strength also occur at this location, giving further support to this interpretation. Tilt studies of the ice flexure caused by tidal variations at locations on either side of this grounding point give additional evidence that grounding is occurring close by. The combination of these three measurements therefore confirms the grounding-line location derived from the satellite imagery and supports the use of this technique to determine grounding.</jats:p> |
| container_start_page |
39 |
| container_title |
Annals of Glaciology |
| container_volume |
20 |
| format_de105 |
Article, E-Article |
| format_de14 |
Article, E-Article |
| format_de15 |
Article, E-Article |
| format_de520 |
Article, E-Article |
| format_de540 |
Article, E-Article |
| format_dech1 |
Article, E-Article |
| format_ded117 |
Article, E-Article |
| format_degla1 |
E-Article |
| format_del152 |
Buch |
| format_del189 |
Article, E-Article |
| format_dezi4 |
Article |
| format_dezwi2 |
Article, E-Article |
| format_finc |
Article, E-Article |
| format_nrw |
Article, E-Article |
| _version_ |
1792345576904327169 |
| geogr_code |
not assigned |
| last_indexed |
2024-03-01T17:25:42.622Z |
| geogr_code_person |
not assigned |
| openURL |
url_ver=Z39.88-2004&ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fvufind.svn.sourceforge.net%3Agenerator&rft.title=Studies+of+the+grounding-line+location+on+Ice+Streams+D+and+E%2C+Antarctica&rft.date=1994-01-01&genre=article&issn=1727-5644&volume=20&spage=39&epage=42&pages=39-42&jtitle=Annals+of+Glaciology&atitle=Studies+of+the+grounding-line+location+on+Ice+Streams+D+and+E%2C+Antarctica&aulast=Bindschadler&aufirst=Robert+A.&rft_id=info%3Adoi%2F10.3189%2F1994aog20-1-39-42&rft.language%5B0%5D=eng |
| SOLR | |
| _version_ | 1792345576904327169 |
| author | Jacobel, Robert W., Robinson, Audrey E., Bindschadler, Robert A. |
| author_facet | Jacobel, Robert W., Robinson, Audrey E., Bindschadler, Robert A., Jacobel, Robert W., Robinson, Audrey E., Bindschadler, Robert A. |
| author_sort | jacobel, robert w. |
| container_start_page | 39 |
| container_title | Annals of Glaciology |
| container_volume | 20 |
| description | <jats:p>Landsat Thematic Mapper (TM) images were used prior to the 1991–92 field season to infer the position of the grounding line at the mouths of Ice Streams D and E, West Antarctica. Our field plan for mass-balance studies was based on this determination, and thus the imagery played a central role in both the scientific and logistics planning. A radar profile along the flow direction was made across the inferred grounding line at one location, and ice-thickness measurements together with surface surveying enable us to compare the hydrostatic surface and the actual topography to determine the point at which the ice becomes grounded. The profile transits from floating to grounded ice at the same location as the grounding line inferred from the imagery. Changes in the radar-echo strength also occur at this location, giving further support to this interpretation. Tilt studies of the ice flexure caused by tidal variations at locations on either side of this grounding point give additional evidence that grounding is occurring close by. The combination of these three measurements therefore confirms the grounding-line location derived from the satellite imagery and supports the use of this technique to determine grounding.</jats:p> |
| doi_str_mv | 10.3189/1994aog20-1-39-42 |
| facet_avail | Online, Free |
| finc_class_facet | Geologie und Paläontologie, Geographie |
| format | ElectronicArticle |
| format_de105 | Article, E-Article |
| format_de14 | Article, E-Article |
| format_de15 | Article, E-Article |
| format_de520 | Article, E-Article |
| format_de540 | Article, E-Article |
| format_dech1 | Article, E-Article |
| format_ded117 | Article, E-Article |
| format_degla1 | E-Article |
| format_del152 | Buch |
| format_del189 | Article, E-Article |
| format_dezi4 | Article |
| format_dezwi2 | Article, E-Article |
| format_finc | Article, E-Article |
| format_nrw | Article, E-Article |
| geogr_code | not assigned |
| geogr_code_person | not assigned |
| id | ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMzE4OS8xOTk0YW9nMjAtMS0zOS00Mg |
| imprint | International Glaciological Society, 1994 |
| imprint_str_mv | International Glaciological Society, 1994 |
| institution | DE-Gla1, DE-Zi4, DE-15, DE-Rs1, DE-Pl11, DE-105, DE-14, DE-Ch1, DE-L229, DE-D275, DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161 |
| issn | 0260-3055, 1727-5644 |
| issn_str_mv | 0260-3055, 1727-5644 |
| language | English |
| last_indexed | 2024-03-01T17:25:42.622Z |
| match_str | jacobel1994studiesofthegroundinglinelocationonicestreamsdandeantarctica |
| mega_collection | International Glaciological Society (CrossRef) |
| physical | 39-42 |
| publishDate | 1994 |
| publishDateSort | 1994 |
| publisher | International Glaciological Society |
| record_format | ai |
| recordtype | ai |
| series | Annals of Glaciology |
| source_id | 49 |
| spelling | Jacobel, Robert W. Robinson, Audrey E. Bindschadler, Robert A. 0260-3055 1727-5644 International Glaciological Society Earth-Surface Processes http://dx.doi.org/10.3189/1994aog20-1-39-42 <jats:p>Landsat Thematic Mapper (TM) images were used prior to the 1991–92 field season to infer the position of the grounding line at the mouths of Ice Streams D and E, West Antarctica. Our field plan for mass-balance studies was based on this determination, and thus the imagery played a central role in both the scientific and logistics planning. A radar profile along the flow direction was made across the inferred grounding line at one location, and ice-thickness measurements together with surface surveying enable us to compare the hydrostatic surface and the actual topography to determine the point at which the ice becomes grounded. The profile transits from floating to grounded ice at the same location as the grounding line inferred from the imagery. Changes in the radar-echo strength also occur at this location, giving further support to this interpretation. Tilt studies of the ice flexure caused by tidal variations at locations on either side of this grounding point give additional evidence that grounding is occurring close by. The combination of these three measurements therefore confirms the grounding-line location derived from the satellite imagery and supports the use of this technique to determine grounding.</jats:p> Studies of the grounding-line location on Ice Streams D and E, Antarctica Annals of Glaciology |
| spellingShingle | Jacobel, Robert W., Robinson, Audrey E., Bindschadler, Robert A., Annals of Glaciology, Studies of the grounding-line location on Ice Streams D and E, Antarctica, Earth-Surface Processes |
| title | Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_full | Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_fullStr | Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_full_unstemmed | Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_short | Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| title_sort | studies of the grounding-line location on ice streams d and e, antarctica |
| title_unstemmed | Studies of the grounding-line location on Ice Streams D and E, Antarctica |
| topic | Earth-Surface Processes |
| url | http://dx.doi.org/10.3189/1994aog20-1-39-42 |