Variability of air temperature over a debris-covered glacier in the Nepalese Himalaya
Estimates of melt from debris-covered glaciers require distributed estimates of meteorological variables and air temperature in particular. Meteorological data are scarce for this environment, and spatial variability of temperature over debris is poorly understood. Based on multiple measurements of...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
International Glaciological Society
2016
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11850/108774 https://doi.org/10.3929/ethz-b-000108774 |
_version_ | 1828055586660417536 |
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author | Steiner, Jakob F. Pellicciotti, Francesca |
author_facet | Steiner, Jakob F. Pellicciotti, Francesca |
author_sort | Steiner, Jakob F. |
collection | ETH Zürich Research Collection |
description | Estimates of melt from debris-covered glaciers require distributed estimates of meteorological variables and air temperature in particular. Meteorological data are scarce for this environment, and spatial variability of temperature over debris is poorly understood. Based on multiple measurements of air and surface temperature from three ablation seasons (2012–14) we investigate the variability of temperature over Lirung Glacier, Nepal, in order to reveal how air temperature is affected by the debris cover and improve ways to extrapolate it. We investigate how much on-glacier temperature deviates from that predicted from a valley lapse rate (LR), analyse on-glacier LRs and test regression models of air temperature and surface temperature. Air temperature over the debris-covered glacier tongue is much higher than what a valley LR would prescribe, so an extrapolation from off-glacier stations is not applicable. An on-glacier LR is clearly defined at night, with strong correlation, but not during the day, when the warming debris disrupts the elevation control. An alternative to derive daytime air temperature is to use a relationship between air and surface temperature, as previously suggested. We find strong variability during daytime that should be accounted for if these regressions are used for temperature extrapolation. ISSN:0260-3055 ISSN:1727-5644 |
format | Article in Journal/Newspaper |
genre | Annals of Glaciology |
genre_facet | Annals of Glaciology |
id | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/108774 |
institution | Open Polar |
language | English |
op_collection_id | ftethz |
op_doi | https://doi.org/20.500.11850/10877410.3929/ethz-b-00010877410.3189/2016AoG71A066 |
op_relation | info:eu-repo/semantics/altIdentifier/doi/10.3189/2016AoG71A066 http://hdl.handle.net/20.500.11850/108774 |
op_rights | info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International |
op_source | Annals of Glaciology, 57 (71) |
publishDate | 2016 |
publisher | International Glaciological Society |
record_format | openpolar |
spelling | ftethz:oai:www.research-collection.ethz.ch:20.500.11850/108774 2025-03-30T14:52:06+00:00 Variability of air temperature over a debris-covered glacier in the Nepalese Himalaya Steiner, Jakob F. Pellicciotti, Francesca 2016-03 application/application/pdf https://hdl.handle.net/20.500.11850/108774 https://doi.org/10.3929/ethz-b-000108774 en eng International Glaciological Society info:eu-repo/semantics/altIdentifier/doi/10.3189/2016AoG71A066 http://hdl.handle.net/20.500.11850/108774 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International Annals of Glaciology, 57 (71) Debris-covered glaciers Energy balance Glacier meteorology Mountain glaciers info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 ftethz https://doi.org/20.500.11850/10877410.3929/ethz-b-00010877410.3189/2016AoG71A066 2025-03-05T22:09:18Z Estimates of melt from debris-covered glaciers require distributed estimates of meteorological variables and air temperature in particular. Meteorological data are scarce for this environment, and spatial variability of temperature over debris is poorly understood. Based on multiple measurements of air and surface temperature from three ablation seasons (2012–14) we investigate the variability of temperature over Lirung Glacier, Nepal, in order to reveal how air temperature is affected by the debris cover and improve ways to extrapolate it. We investigate how much on-glacier temperature deviates from that predicted from a valley lapse rate (LR), analyse on-glacier LRs and test regression models of air temperature and surface temperature. Air temperature over the debris-covered glacier tongue is much higher than what a valley LR would prescribe, so an extrapolation from off-glacier stations is not applicable. An on-glacier LR is clearly defined at night, with strong correlation, but not during the day, when the warming debris disrupts the elevation control. An alternative to derive daytime air temperature is to use a relationship between air and surface temperature, as previously suggested. We find strong variability during daytime that should be accounted for if these regressions are used for temperature extrapolation. ISSN:0260-3055 ISSN:1727-5644 Article in Journal/Newspaper Annals of Glaciology ETH Zürich Research Collection |
spellingShingle | Debris-covered glaciers Energy balance Glacier meteorology Mountain glaciers Steiner, Jakob F. Pellicciotti, Francesca Variability of air temperature over a debris-covered glacier in the Nepalese Himalaya |
title | Variability of air temperature over a debris-covered glacier in the Nepalese Himalaya |
title_full | Variability of air temperature over a debris-covered glacier in the Nepalese Himalaya |
title_fullStr | Variability of air temperature over a debris-covered glacier in the Nepalese Himalaya |
title_full_unstemmed | Variability of air temperature over a debris-covered glacier in the Nepalese Himalaya |
title_short | Variability of air temperature over a debris-covered glacier in the Nepalese Himalaya |
title_sort | variability of air temperature over a debris-covered glacier in the nepalese himalaya |
topic | Debris-covered glaciers Energy balance Glacier meteorology Mountain glaciers |
topic_facet | Debris-covered glaciers Energy balance Glacier meteorology Mountain glaciers |
url | https://hdl.handle.net/20.500.11850/108774 https://doi.org/10.3929/ethz-b-000108774 |