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6 results for “Debris temperature”
Debris temperature and ablation measurements from the Lirung Debris-Covered Glacier (2013-2014), Nepal
<p>These data are from the debris-covered portion of Lirung Glacier, Langtang Valley located in the Langtang National Park of the Nepal Himalaya that were collected during three field expeditions between September 2013 and April 2014. The data includes debris temperature measurements at two different sites of the glacier in three different seasons of the year 2013 (Monsoon and Winter) and 2014 (Pre-Monsoon). Debris temperature measurements from thermistors located at the surface (Black-colored dirty ice) to up to 40 cm from the surface. Dataset also included the ablation measurement in three seasons at different debris-thicknesses. Below is a brief description of the two different datasets:</p> <p>- Ablation_stake_data_Lirung_glacier_CHAND.csv: ablation stake measurement in the Monsoon and Winter season of 2013 and pre-monsoon season of 2014 from Chand and Kayastha (2018) and Chand et al. (2015).</p> <p>- Debris_temperature_profile_Lirung_Glacier_CHAND.csv: debris temperature measurements (Degree Celcius) where the depth is reported in cm from Chand and Kayastha (2018).</p> <p>----- Citing datasets -----</p> <p>Chand, M. B., and Kayastha, R. B. (2018). Study of thermal properties of supraglacial debris and degree-day factors on Lirung Glacier, Nepal. Sciences in Cold and Arid Regions, 10(5): 357-368 doi:10.3724/SP.J.1226.2018.00357</p> <p>Chand, M. B., Kayastha, R. B., Parajuli, A., and Mool, P. K. (2015). Seasonal variation of ice melting on varying layers of the debris of Lirung Glacier, Langtang Valley, Nepal, Proc. IAHS, 368, 21–26, https://doi.org/10.5194/piahs-368-21-2015</p> <p> </p>
On-Glacier Air Temperatures for Miage Debris-Covered Glacier, 2014
<p>Miage_Glacier_Air_Temperature_Data_2014.xlsx<br> %------------------------------------------%<br> Data Generated on 13th May 2022</p> <p>Data Curator: Dr. Thomas Shaw (Swiss Federal Institute, WSL, Switzerland)</p> <p>Data Provider(s): Dr. Thomas Shaw (Swiss Federal Institute, WSL, Switzerland) thomas.shaw@wsl.ch<br> Prof. Benjamin Brock (Northumbria University, Newcastle, UK) benjamin.brock@northumbria.ac.uk</p> <p>Data period: 1st July - 27th September, 2014</p> <p><br> Details:<br> Hourly data are generated for air temperature stations ('T-Loggers') distributed across the debris-covered Miage Glacier, Italy (45.8129°N, 6.8458°E).<br> Air temperatures (°C) were measured using Tinytag thermistors (accuracy +/- 0.2-0.35°C) housed in naturally ventilated Campbell MET20 / MET21 radiation shields.</p> <p>Off-Glacier air temperatures (measured as above) are provided for comparison with on-glacier air temperatures. </p> <p>For additional details can be found in the article: <br> Shaw, T. E., Brock, B. W., Fyffe, C. L., Pellicciotti, F., Rutter, N., & Diotri, F. (2016).<br> Air temperature distribution and energy-balance modelling of a debris-covered glacier. Journal of Glaciology, 62(231), 1–14. <br> https://doi.org/10.1017//jog.2016.31</p> <p>Please cite the above article for any usage of the dataset.</p> <p>Data are shared and compiled as part of a wider project to estimate on-glacier air temperatures from off-glacier data<br> For more details on the 'TEMPEST' project, visit: https://tempestglacier.com/</p>
Supraglacial debris temperature measurements from Ngozumpa Glacier, Nepal (2001–2002)
<p>Supraglacial debris temperature measurements from a site 1.5 km from the terminus of Ngozumpa Glacier, Nepal, collected between 13 November 2001 and 12 October 2002. Debris temperatures were measured every 30 minutes at six thermistors within the debris layer at depths of 0.0 m, 0.22 m, 0.33 m, 0.45 m, 0.65 m and 0.77 m from the debris surface. The estimated thickness of the debris layer at this site was 2.20 m.</p> <p>Measurements were made using Gemini thermistors and Tinytag Plus TGP-0073 loggers with a stated accuracy of ±0.3°C at 0°C.</p> <p>These data were first presented in: Nicholson L and Benn DI (2013) Properties of natural supraglacial debris in relation to modelling sub‐debris ice ablation. <em>Earth Surface Processes and Landforms</em> 38(5), 490–501 (doi:10.1002/esp.3299)</p> <p> </p> <p> </p> <div class="wayback1996-RTmodal"> <div> </div> <div> </div> × <div> </div> <div> </div> <div> </div> </div>
Polyethylene tarping elevates temperature and reduces emergence of <em>Phloeosinus punctatus</em> LeConte (Coleoptera: Curculionidae) from giant sequoia debris piles
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Temperature profile measurements in the debris-covered headwalls of four thaw slumps in the Tuktoyaktuk Coastlands, Northwest Territories, Canada
<p>Temperature profile measurements in the debris-covered headwalls of four thaw slumps in the Tuktoyaktuk Coastlands, Northwest Territories, Canada, summer 2018</p> <p>Instruments<br> We used iButton probes (DS1922L; maxim integrated) that were coated with resin.<br> We submerged the probes in an ice bath from 2018-5-31 22:00 - 2018-06-01 11:00.</p> <p>Deployment<br> The iButtons were anchored in hollow, sealed rods. The rods were inserted so that iButtons were located at 5, 20 and 35 cm depth.<br> The rods contained the following iButtons at (05, 20, 35) cm depth [None indicating that there was no probe in the respective slot]:<br> Rod, (probe at 5 cm, probe at 20 cm, probe at 35 cm),<br> 1, (01,02,03)<br> 2, (None,04,None)<br> 3, (None,05,None)<br> 4, (06,07,08)<br> 5, (09,10,11)<br> 6, (None,12,None)<br> 7, (None,13,None)<br> 8, (None,14,None)<br> 9, (16,15,None)<br> 10, (17,18,19)</p> <p>Locations<br> Top Lake:<br> Location: 68.757N, 133.520W<br> Rods: 4 (central), 7 (23 cm above central rod in dip direction), 1 (25 cm from central rod in strike direction [west]), 6 (23 cm below central rod in dip direction), 20 (10 m from headwall; slump floor)<br> Deployment: 2018-06-15 - 2018-08-05</p> <p> Evan Lake:<br> Location: 68.754N, 133.464W<br> Rods: 9 (central)<br> Deployment: 2018-06-13 - 2018-08-24</p> <p> Roadside:<br> Location: 69.007N, 133.361W<br> Rods: 10 (central), 2 (20 cm above central rod in dip direction), 8 (20 cm from central rod in strike direction [west]), 3 (20 cm below central rod in dip direction)<br> Deployment: 2018-06-27 - 2018-08-21</p> <p> Timbit Lake:<br> Location: 69.105N, 133.290W<br> Rods: 5 (central)<br> Deployment: 2018-06-15 - lost<br> <br> Data description:<br> Each XX.txt file contains the native output of the iButton software by maxim integrated for probe XX. A calibration offset can be estimated from the average temperature recorded during the ice-bath calibration period.</p>
Supraglacial debris temperature measurements from Ngozumpa Glacier, Nepal (2014–2016)
<p>Supraglacial debris temperature measurements from a site 1.6 km from the terminus of Ngozumpa Glacier, Nepal, collected between 06 December 2014 and 03 April 2016. Debris temperatures were measured every six hours at 11 thermistors within the debris layer at depths of 0.01 m, 0.2 m, 0.4 m, 0.6 m, 0.8 m, 1.0 m, 1.2 m, 1.4 m, 1.6 m, 1.8 m and 2.0 m from the debris surface. The thickness of the debris layer at this site was 2.0 m, and the lowermost thermistor was installed at the debris-ice interface.</p> <p>Measurements were made using a Geoprecision thermistor array with a stated accuracy of ±0.25°C.</p> <div class="wayback1996-RTmodal"> <div> </div> <div> </div> × <div> </div> <div> </div> <div> </div> </div>
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