• No results found

[PDF] Top 20 Supraglacial debris thickness variability: impact on ablation and relation to terrain properties

Has 10000 "Supraglacial debris thickness variability: impact on ablation and relation to terrain properties" found on our website. Below are the top 20 most common "Supraglacial debris thickness variability: impact on ablation and relation to terrain properties".

Supraglacial debris thickness variability: impact on ablation and relation to terrain properties

Supraglacial debris thickness variability: impact on ablation and relation to terrain properties

... surface debris temperature for the stated inputs, as a function of debris ...for variability in surface energy receipts due to local or surround- ing terrain, or the effects of spatially or ... See full document

16

Changes in glacier surface cover on Baltoro Glacier, Karakoram, North Pakistan, 2001 to 2012

Changes in glacier surface cover on Baltoro Glacier, Karakoram, North Pakistan, 2001 to 2012

... 2010). Supraglacial debris thickness for the entire gla- cier was calculated by Mihalcea et ...potential impact of spatial differences in thermal energy stored in the debris due to ... See full document

10

Supraglacial ponds regulate runoff from Himalayan debris covered glaciers

Supraglacial ponds regulate runoff from Himalayan debris covered glaciers

... a supraglacial debris mantle present on many of the region ’ s glaciers, which cov- ers up to 36% of the glacierized area in the Everest region (Bolch et ...This debris mantle commonly causes ... See full document

12

Supraglacial Ponds Regulate Runoff From Himalayan Debris‐Covered Glaciers

Supraglacial Ponds Regulate Runoff From Himalayan Debris‐Covered Glaciers

... a supraglacial debris mantle present on many of the region ’ s glaciers, which cov- ers up to 36% of the glacierized area in the Everest region (Bolch et ...This debris mantle commonly causes ... See full document

11

Variations in near‐surface debris temperature through the summer monsoon on Khumbu Glacier, Nepal Himalaya

Variations in near‐surface debris temperature through the summer monsoon on Khumbu Glacier, Nepal Himalaya

... and debris characteristics such as moisture content, porosity, lithology and thermal conductivity would increase the accuracy of results using the surface energy balance ...and debris properties on a ... See full document

17

Changes in glacier surface cover on Baltoro glacier, Karakoram, north Pakistan, 2001–2012

Changes in glacier surface cover on Baltoro glacier, Karakoram, north Pakistan, 2001–2012

... 2010). Supraglacial debris thickness for the entire gla- cier was calculated by Mihalcea et ...potential impact of spatial differences in thermal energy stored in the debris due to ... See full document

10

Debris-covered glacier energy balance model for Imja–Lhotse Shar Glacier in the Everest region of Nepal

Debris-covered glacier energy balance model for Imja–Lhotse Shar Glacier in the Everest region of Nepal

... the debris is ...of debris should be much lower than solid rock due to the pore spaces being filled with air and ...the debris and its influence on the thermal ...the debris to be computed at ... See full document

16

Unravelling the evolution of Zmuttgletscher and its debris cover since the end of the Little Ice Age

Unravelling the evolution of Zmuttgletscher and its debris cover since the end of the Little Ice Age

... the debris-covered area increased from ...increasing debris extent as they lead to a rise of the rain–snow transition altitude as well as higher ice ...Therefore, debris emergence accelerates and ... See full document

21

Impact of frontal ablation on the ice thickness estimation of marine-terminating glaciers in Alaska

Impact of frontal ablation on the ice thickness estimation of marine-terminating glaciers in Alaska

... in thickness along the main centre line, with and without ac- counting for frontal ablation, are not relevant for the po- tential glacier contribution to sea-level rise, since most of the differences in ... See full document

16

Structure and evolution of the drainage system of a Himalayan debris covered glacier, and its relationship with patterns of mass loss

Structure and evolution of the drainage system of a Himalayan debris covered glacier, and its relationship with patterns of mass loss

... upper ablation zone are too large to be explained by changes in ice creep rates, which would require fluctuations in driving stress that are inconsistent with the observed surface elevation changes on the glacier ... See full document

18

Detumbling large space debris via laser ablation

Detumbling large space debris via laser ablation

... space debris (the target) before the spacecraft starts deflecting its trajectory through laser ...the debris is estimated through the application of the optic flow ... See full document

10

Supraglacial forcing of subglacial drainage in the ablation zone of the Greenland ice sheet

Supraglacial forcing of subglacial drainage in the ablation zone of the Greenland ice sheet

... of supraglacial melt extent results in the upglacier expansion of the efficient subglacial drainage system through the delivery of surface meltwater to the glacier bed [ Nienow et ... See full document

5

Surface lowering of the debris-covered area of Kanchenjunga Glacier in the eastern Nepal Himalaya since 1975, as revealed by Hexagon KH-9 and ALOS satellite observations

Surface lowering of the debris-covered area of Kanchenjunga Glacier in the eastern Nepal Himalaya since 1975, as revealed by Hexagon KH-9 and ALOS satellite observations

... studied debris-covered glacier in the Himalayas, and is ex- periencing a greater degree of mass loss than Kanchenjunga Glacier, with a mass balance of − ...and debris-covered areas and (2) varying density ... See full document

13

Biomechanics and energetics of walking on uneven terrain

Biomechanics and energetics of walking on uneven terrain

... complex terrain in their everyday ...unclear. Terrain has many features that might affect locomotion, such as height variations, damping and coefficient of ...natural terrain can affect locomotion, ... See full document

8

Rheological investigation and simulation of a debris-flow event in the Fella watershed

Rheological investigation and simulation of a debris-flow event in the Fella watershed

... 6. The effect, not negligible, like Sosio et al. (2006) says, of the frictional component owing to the coarse fraction that is not possible to include in the laboratory analy- sis. This means that there is an ... See full document

9

Incorporating Distributed Debris Thickness in a Glacio-Hydrological Model: Khumbu Himalaya, Nepal

Incorporating Distributed Debris Thickness in a Glacio-Hydrological Model: Khumbu Himalaya, Nepal

... The lack of multiple calibration data sets, for example, volume change and snow accumulation, create problems in terms of the cause of volume changes. For example, correct volume loss can be attained through incorrect ... See full document

35

An example of debris-flows hazard modeling using GIS

An example of debris-flows hazard modeling using GIS

... predicting debris-flows ...in relation to ...between debris-flows and the various causative factors provides new understand- ing of the ...potential debris-flow source ...most ... See full document

12

Impact of varying debris cover thickness on ablation: a case study for Koxkar Glacier in the Tien Shan

Impact of varying debris cover thickness on ablation: a case study for Koxkar Glacier in the Tien Shan

... 2010b). Debris thickness ranges from less than ...the ablation area and on ice-cliff slopes to more than 3 m ...an ablation zone of about ... See full document

10

Automated detection of ice cliffs within supraglacial debris cover

Automated detection of ice cliffs within supraglacial debris cover

... “thin” debris covering true ice ...% debris- ...% debris cover should have a distinguishable signal, but this is a best case in both pixel/ice cliff location coincidence and fraction of “thin” ... See full document

19

Modelling debris transport within glaciers by advection in a full-Stokes ice flow model

Modelling debris transport within glaciers by advection in a full-Stokes ice flow model

... surface debris cover respond differently to climate forcing than those with- out supraglacial ...include debris-covered glaciers in projections of glaciogenic runoff and sea level rise and to ... See full document

16

Show all 10000 documents...