Articles | Volume 10, issue 1
https://doi.org/10.5194/tc-10-133-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-10-133-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
18 Jan 2016
Research article |
| 18 Jan 2016
Climatic controls and climate proxy potential of Lewis Glacier, Mt. Kenya
Department of Geography and Regional Science, University of Graz, Heinrichstraße 36, 8010 Graz, Austria
Institute of Atmospheric and Cryospheric Sciences, until May 2015 known as the Institute of Meteorology and Geophysics, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria
L. I. Nicholson
Institute of Atmospheric and Cryospheric Sciences, until May 2015 known as the Institute of Meteorology and Geophysics, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria
Institute of Geography, Friedrich-Alexander University Erlangen-Nürnberg (FAU), Wetterkreuz 15, 91058 Erlangen, Germany
W. Gurgiser
Institute of Atmospheric and Cryospheric Sciences, until May 2015 known as the Institute of Meteorology and Geophysics, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria
G. Kaser
Institute of Atmospheric and Cryospheric Sciences, until May 2015 known as the Institute of Meteorology and Geophysics, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria
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Cited
19 citations as recorded by crossref.
- Future changes in climate extremes over Equatorial East Africa based on CMIP5 multimodel ensemble V. Ongoma et al. 10.1007/s11069-017-3079-9
- Uncertainty assessment of a permanent long-range terrestrial laser scanning system for the quantification of snow dynamics on Hintereisferner (Austria) A. Voordendag et al. 10.3389/feart.2023.1085416
- Robust uncertainty assessment of the spatio-temporal transferability of glacier mass and energy balance models T. Zolles et al. 10.5194/tc-13-469-2019
- Perceptions of Ecosystem Services and Climate Change in the Communities Surrounding Mt. Kenya and Mt. Elgon, Kenya T. Downing et al. 10.3390/su151411470
- A comparison of simultaneous temperature and humidity observations from the SW and NE slopes of Kilimanjaro: The role of slope aspect and differential land-cover in controlling mountain climate N. Pepin et al. 10.1016/j.gloplacha.2017.08.006
- Glacier variations and rising temperature in the Mt. Kenya since the Last Glacial Maximum A. Chen et al. 10.1007/s11629-017-4600-z
- Mesoscale atmospheric circulation controls of local meteorological elevation gradients on Kersten Glacier near Kilimanjaro summit T. Mölg et al. 10.5194/esd-11-653-2020
- The freezing level in the tropical Andes, Peru: An indicator for present and future glacier extents S. Schauwecker et al. 10.1002/2016JD025943
- Mapping the Loss of Mt. Kenya’s Glaciers: An Example of the Challenges of Satellite Monitoring of Very Small Glaciers R. Prinz et al. 10.3390/geosciences8050174
- Evaluation of different methods to model near-surface turbulent fluxes for a mountain glacier in the Cariboo Mountains, BC, Canada V. Radić et al. 10.5194/tc-11-2897-2017
- Tropical glacier loss in East Africa: recent areal extents on Kilimanjaro, Mount Kenya, and in the Rwenzori Range from high-resolution remote sensing data A. Hinzmann et al. 10.1088/2752-5295/ad1fd7
- Climate Controls on the Interseasonal and Interannual Variability of the Surface Mass and Energy Balances of a Tropical Glacier (Zongo Glacier, Bolivia, 16°S): New Insights From the Multi‐Year Application of a Distributed Energy Balance Model P. Autin et al. 10.1029/2021JD035410
- Spatial Distribution of Unique Biological Communities and Their Control Over Surface Reflectivity of the Stanley Glacier, Uganda J. Uetake et al. 10.3389/feart.2022.740998
- Energy and mass balance characteristics of the Guliya ice cap in the West Kunlun Mountains, Tibetan Plateau S. Li et al. 10.1016/j.coldregions.2018.12.001
- New insights into the decadal variability in glacier volume of a tropical ice cap, Antisana (0°29′ S, 78°09′ W), explained by the morpho-topographic and climatic context R. Basantes-Serrano et al. 10.5194/tc-16-4659-2022
- Effects of local advection on the spatial sensible heat flux variation on a mountain glacier T. Sauter & S. Galos 10.5194/tc-10-2887-2016
- Spatio-temporal flow variations driving heat exchange processes at a mountain glacier R. Mott et al. 10.5194/tc-14-4699-2020
- Validation of simulated temperature profiles at rock walls in the eastern alps (Dachstein) H. Schnepfleitner et al. 10.1002/ppp.1962
- Accelerated glacier mass loss with atmospheric changes on Mt. Yulong, Southeastern Tibetan Plateau X. Yan et al. 10.1016/j.jhydrol.2021.126931
19 citations as recorded by crossref.
- Future changes in climate extremes over Equatorial East Africa based on CMIP5 multimodel ensemble V. Ongoma et al. 10.1007/s11069-017-3079-9
- Uncertainty assessment of a permanent long-range terrestrial laser scanning system for the quantification of snow dynamics on Hintereisferner (Austria) A. Voordendag et al. 10.3389/feart.2023.1085416
- Robust uncertainty assessment of the spatio-temporal transferability of glacier mass and energy balance models T. Zolles et al. 10.5194/tc-13-469-2019
- Perceptions of Ecosystem Services and Climate Change in the Communities Surrounding Mt. Kenya and Mt. Elgon, Kenya T. Downing et al. 10.3390/su151411470
- A comparison of simultaneous temperature and humidity observations from the SW and NE slopes of Kilimanjaro: The role of slope aspect and differential land-cover in controlling mountain climate N. Pepin et al. 10.1016/j.gloplacha.2017.08.006
- Glacier variations and rising temperature in the Mt. Kenya since the Last Glacial Maximum A. Chen et al. 10.1007/s11629-017-4600-z
- Mesoscale atmospheric circulation controls of local meteorological elevation gradients on Kersten Glacier near Kilimanjaro summit T. Mölg et al. 10.5194/esd-11-653-2020
- The freezing level in the tropical Andes, Peru: An indicator for present and future glacier extents S. Schauwecker et al. 10.1002/2016JD025943
- Mapping the Loss of Mt. Kenya’s Glaciers: An Example of the Challenges of Satellite Monitoring of Very Small Glaciers R. Prinz et al. 10.3390/geosciences8050174
- Evaluation of different methods to model near-surface turbulent fluxes for a mountain glacier in the Cariboo Mountains, BC, Canada V. Radić et al. 10.5194/tc-11-2897-2017
- Tropical glacier loss in East Africa: recent areal extents on Kilimanjaro, Mount Kenya, and in the Rwenzori Range from high-resolution remote sensing data A. Hinzmann et al. 10.1088/2752-5295/ad1fd7
- Climate Controls on the Interseasonal and Interannual Variability of the Surface Mass and Energy Balances of a Tropical Glacier (Zongo Glacier, Bolivia, 16°S): New Insights From the Multi‐Year Application of a Distributed Energy Balance Model P. Autin et al. 10.1029/2021JD035410
- Spatial Distribution of Unique Biological Communities and Their Control Over Surface Reflectivity of the Stanley Glacier, Uganda J. Uetake et al. 10.3389/feart.2022.740998
- Energy and mass balance characteristics of the Guliya ice cap in the West Kunlun Mountains, Tibetan Plateau S. Li et al. 10.1016/j.coldregions.2018.12.001
- New insights into the decadal variability in glacier volume of a tropical ice cap, Antisana (0°29′ S, 78°09′ W), explained by the morpho-topographic and climatic context R. Basantes-Serrano et al. 10.5194/tc-16-4659-2022
- Effects of local advection on the spatial sensible heat flux variation on a mountain glacier T. Sauter & S. Galos 10.5194/tc-10-2887-2016
- Spatio-temporal flow variations driving heat exchange processes at a mountain glacier R. Mott et al. 10.5194/tc-14-4699-2020
- Validation of simulated temperature profiles at rock walls in the eastern alps (Dachstein) H. Schnepfleitner et al. 10.1002/ppp.1962
- Accelerated glacier mass loss with atmospheric changes on Mt. Yulong, Southeastern Tibetan Plateau X. Yan et al. 10.1016/j.jhydrol.2021.126931
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Latest update: 18 Apr 2024
Short summary
Lewis Glacier has lost > 80 % of its extent since the late 19th century. A sensitivity study using a process-based model assigns this shrinking to decreased atmospheric moisture without increasing air temperatures required. The glacier retreat implies a distinctly different coupling between the glacier's surface-air layer and its surrounding boundary layer, underlining the difficulty of deriving palaeoclimates for larger glacier extents on the basis of modern measurements of small glaciers.
Lewis Glacier has lost 80 % of its extent since the late 19th century. A sensitivity study...
