Snow accumulation across Ekströmisen and Ritscherflya

Snow accumulation is an important glaciological parameter for various kinds of studies in Antarctica. A traverse route runs from Neumayer station (70° 38.6S, 8° 15.5W) at the coast across Ekströmisen and Ritscherflya towards Kottasberge, Heimefrontfjella (Kottas camp 74° 12.3S, 9° 44.8W). This 410 k...

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Main Author: Oerter, Hans
Format: Conference Object
Language:unknown
Published: 2003
Subjects:
Online Access:https://epic.awi.de/id/eprint/6106/
https://hdl.handle.net/10013/epic.16656
id ftawi:oai:epic.awi.de:6106
record_format openpolar
spelling ftawi:oai:epic.awi.de:6106 2023-09-05T13:15:24+02:00 Snow accumulation across Ekströmisen and Ritscherflya Oerter, Hans 2003 https://epic.awi.de/id/eprint/6106/ https://hdl.handle.net/10013/epic.16656 unknown Oerter, H. (2003) Snow accumulation across Ekströmisen and Ritscherflya , 21. Internationale Polartagung, Deutsche Gesellschaft für Polarforschung, Kiel, 17 March 2003 - 22 March 2003 . hdl:10013/epic.16656 EPIC321. Internationale Polartagung, Deutsche Gesellschaft für Polarforschung, Kiel, 2003-03-17-2003-03-22 Conference notRev 2003 ftawi 2023-08-22T19:45:53Z Snow accumulation is an important glaciological parameter for various kinds of studies in Antarctica. A traverse route runs from Neumayer station (70° 38.6S, 8° 15.5W) at the coast across Ekströmisen and Ritscherflya towards Kottasberge, Heimefrontfjella (Kottas camp 74° 12.3S, 9° 44.8W). This 410 km long route was marked in 1985/86 for the first time by bamboo stakes with a spacing of 500 m as route markers. From the beginning the stakes were used for accumulation studies as well. The stake line was re-established in the 1996/97 season starting at a waypoint in 9 km distance from the Neumayer station. Since then it was read and maintained each year. Only with the availability of GPS it was possible to locate the stakes precisely enough to correlate unambiguously the readings of two successive years. The accumulation profile shows great variability depending on surface topography and wind field. There are also considerable yearly variations. Near surface density (0-1 m depth) values obtained from snow pit studies allow to convert the stake readings to accumulation values in water equivalent units.The traverse route was subdivided into 9 sections. Section 1 represents the ice shelf area from the starting point (9 km distance to Neumayer station) to waypoint 70 km, section 2 the remaining ice shelf area to the grounding line, section 3 the first 48 km of the ascend to Ritscherflya. Sections 4, 5 and 6 are the next 45, 55, and 45 km, respectively. Section 7 represents the remaining 94 km towards Kottas camp, in front of Kottasberge. Section 8 runs from Kottas camp to Strømmebakken, the gate to cross Kottasberge. Section 9, finally, runs along Strømmebakken towards Amundsenisen. In total the stake line is 454 km long and in the 2001/02 season 911 stakes were used to calculate accumulation rates. The table shows the results for the 5years period 1997-2001: Distance along the 9 profile sections, the measured change in snow height related to a 1-year period and averaged for each section, the mean near surface density, ... Conference Object Antarc* Antarctica Ice Shelf Polarforschung Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Amundsenisen ENVELOPE(-6.000,-6.000,-74.500,-74.500) Ekströmisen ENVELOPE(-8.000,-8.000,-71.000,-71.000) Heimefrontfjella ENVELOPE(-11.000,-11.000,-74.667,-74.667) Kottasberge ENVELOPE(-9.750,-9.750,-74.333,-74.333) Neumayer Neumayer Station Ritscherflya ENVELOPE(-9.000,-9.000,-73.000,-73.000) Strømmebakken ENVELOPE(-9.133,-9.133,-74.303,-74.303) The Gate ENVELOPE(-124.937,-124.937,61.417,61.417)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Snow accumulation is an important glaciological parameter for various kinds of studies in Antarctica. A traverse route runs from Neumayer station (70° 38.6S, 8° 15.5W) at the coast across Ekströmisen and Ritscherflya towards Kottasberge, Heimefrontfjella (Kottas camp 74° 12.3S, 9° 44.8W). This 410 km long route was marked in 1985/86 for the first time by bamboo stakes with a spacing of 500 m as route markers. From the beginning the stakes were used for accumulation studies as well. The stake line was re-established in the 1996/97 season starting at a waypoint in 9 km distance from the Neumayer station. Since then it was read and maintained each year. Only with the availability of GPS it was possible to locate the stakes precisely enough to correlate unambiguously the readings of two successive years. The accumulation profile shows great variability depending on surface topography and wind field. There are also considerable yearly variations. Near surface density (0-1 m depth) values obtained from snow pit studies allow to convert the stake readings to accumulation values in water equivalent units.The traverse route was subdivided into 9 sections. Section 1 represents the ice shelf area from the starting point (9 km distance to Neumayer station) to waypoint 70 km, section 2 the remaining ice shelf area to the grounding line, section 3 the first 48 km of the ascend to Ritscherflya. Sections 4, 5 and 6 are the next 45, 55, and 45 km, respectively. Section 7 represents the remaining 94 km towards Kottas camp, in front of Kottasberge. Section 8 runs from Kottas camp to Strømmebakken, the gate to cross Kottasberge. Section 9, finally, runs along Strømmebakken towards Amundsenisen. In total the stake line is 454 km long and in the 2001/02 season 911 stakes were used to calculate accumulation rates. The table shows the results for the 5years period 1997-2001: Distance along the 9 profile sections, the measured change in snow height related to a 1-year period and averaged for each section, the mean near surface density, ...
format Conference Object
author Oerter, Hans
spellingShingle Oerter, Hans
Snow accumulation across Ekströmisen and Ritscherflya
author_facet Oerter, Hans
author_sort Oerter, Hans
title Snow accumulation across Ekströmisen and Ritscherflya
title_short Snow accumulation across Ekströmisen and Ritscherflya
title_full Snow accumulation across Ekströmisen and Ritscherflya
title_fullStr Snow accumulation across Ekströmisen and Ritscherflya
title_full_unstemmed Snow accumulation across Ekströmisen and Ritscherflya
title_sort snow accumulation across ekströmisen and ritscherflya
publishDate 2003
url https://epic.awi.de/id/eprint/6106/
https://hdl.handle.net/10013/epic.16656
long_lat ENVELOPE(-6.000,-6.000,-74.500,-74.500)
ENVELOPE(-8.000,-8.000,-71.000,-71.000)
ENVELOPE(-11.000,-11.000,-74.667,-74.667)
ENVELOPE(-9.750,-9.750,-74.333,-74.333)
ENVELOPE(-9.000,-9.000,-73.000,-73.000)
ENVELOPE(-9.133,-9.133,-74.303,-74.303)
ENVELOPE(-124.937,-124.937,61.417,61.417)
geographic Amundsenisen
Ekströmisen
Heimefrontfjella
Kottasberge
Neumayer
Neumayer Station
Ritscherflya
Strømmebakken
The Gate
geographic_facet Amundsenisen
Ekströmisen
Heimefrontfjella
Kottasberge
Neumayer
Neumayer Station
Ritscherflya
Strømmebakken
The Gate
genre Antarc*
Antarctica
Ice Shelf
Polarforschung
genre_facet Antarc*
Antarctica
Ice Shelf
Polarforschung
op_source EPIC321. Internationale Polartagung, Deutsche Gesellschaft für Polarforschung, Kiel, 2003-03-17-2003-03-22
op_relation Oerter, H. (2003) Snow accumulation across Ekströmisen and Ritscherflya , 21. Internationale Polartagung, Deutsche Gesellschaft für Polarforschung, Kiel, 17 March 2003 - 22 March 2003 . hdl:10013/epic.16656
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