Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Ben W. Brock"'
Autor:
Grace L. Brown, Ben W. Brock
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
The cryosphere plays an important role in the global carbon cycle, but few studies have examined carbon fluxes specifically on debris-covered glaciers. To improve understanding of the magnitude and variability of the atmospheric carbon flux in suprag
Externí odkaz:
https://doaj.org/article/310dff99c7154fa59cc559612be9b3f7
Autor:
Patrick Troxler, Álvaro Ayala, Thomas E. Shaw, Matt Nolan, Ben W. Brock, Francesca Pellicciotti
Publikováno v:
Journal of Glaciology, Vol 66, Pp 386-400 (2020)
We examine the spatial patterns of near-surface air temperature (Ta) over a melting glacier using a multi-annual dataset from McCall Glacier, Alaska. The dataset consists of a 10-year (2005–2014) meteorological record along the glacier centreline u
Externí odkaz:
https://doaj.org/article/a381dabf294049c098887d6d42f0c47b
Publikováno v:
Journal of Glaciology, Vol 63, Pp 973-988 (2017)
The spatio-temporal distribution of air temperature over mountain glaciers can demonstrate complex patterns, yet it is often represented simplistically using linear vertical temperature gradients (VTGs) extrapolated from off-glacier locations. We ana
Externí odkaz:
https://doaj.org/article/47c9f9c2bb3f466993a4206d7a15de5d
Autor:
Yu Zhu, Shiyin Liu, Ben W. Brock, Lide Tian, Ying Yi, Fuming Xie, Donghui Shangguan, YiYuan Shen
Publikováno v:
Hydrology & Earth System Sciences Discussions; 11/6/2023, p1-25, 25p
Publikováno v:
Hydrological Processes. 34:3738-3757
The Irtysh River is the main water resource of Eastern Kazakhstan and its upper basin is severely affected by spring floods each year, primarily as a result of snowmelt. Knowledge of the large‐scale processes that influence the timing of these snow
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6dec2a3e3017cf1b1d6f4ce5b6b4a735
https://doi.org/10.1002/hyp.13843
https://doi.org/10.1002/hyp.13843
Autor:
Matthew J. Westoby, Catriona Fyffe, Peter L. Moore, Thomas E. Shaw, Rebecca Stewart, Ben W. Brock, David R. Rounce
In the last decade or so, improvements in unpiloted aerial systems (UAS) technology and the emergence of low-cost digital photogrammetry have democratised access to accurate, high-resolution topographic data products, particularly in remote, glacial
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dad17ea5ecd7ace3006c74d1ed9891de
https://doi.org/10.5194/egusphere-egu2020-8475
https://doi.org/10.5194/egusphere-egu2020-8475
Autor:
Alvaro Ayala, Matt Nolan, Francesca Pellicciotti, Ben W. Brock, Thomas E. Shaw, Patrick Troxler
Publikováno v:
Journal of Glaciology, 66 (257)
We examine the spatial patterns of near-surface air temperature (Ta) over a melting glacier using a multi-annual dataset from McCall Glacier, Alaska. The dataset consists of a 10-year (2005–2014) meteorological record along the glacier centreline u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::66bb5820797248d1e9e22dda5bb90519
Publikováno v:
Geomorphology. 97:24-34
A key problem in understanding valley evolution in alpine landscapes has been the lack of an independent timescale against which to measure morphological change. Here, we outline that by using space as a proxy for time, the role of glaciation in prod
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c253c7de98b863cfa8390e06d5708b5
https://doi.org/10.1016/j.geomorph.2007.02.036
https://doi.org/10.1016/j.geomorph.2007.02.036
Publikováno v:
Earth Surface Processes and Landforms. 31:1167-1175
The intractable obstacle to understanding cirque evolution has been the lack of an independent timescale against which to measure morphometric change. By using known rates of transport and uplift of the Southern Alps, combined with the oxygen isotope
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::30c9ae17b20f2fa77cb0a4f6ef37c787
https://doi.org/10.1002/esp.1327
https://doi.org/10.1002/esp.1327
Publikováno v:
Journal of Glaciology. 52:281-297
Spatial and temporal variations in aerodynamic roughness length (z0) on Haut Glacier d’Arolla, Switzerland, during the 1993 and 1994 ablation seasons are described, based on measurements of surface microtopography. The validity of the microtopograp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b0ec958b732f9fedb198b83e0015243d
https://doi.org/10.3189/172756506781828746
https://doi.org/10.3189/172756506781828746