Zobrazeno 1 - 9
of 9
pro vyhledávání: '"T. D. L. IRVINE-FYNN"'
Autor:
T. D. L. Irvine-Fynn, A. Edwards, I. T. Stevens, A. C. Mitchell, P. Bunting, J. E. Box, K. A. Cameron, J. M. Cook, K. Naegeli, S. M. E. Rassner, J. C. Ryan, M. Stibal, C. J. Williamson, A. Hubbard
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-11 (2021)
Microbes that colonise ice sheet surfaces are important to the carbon cycle, but their biomass and transport remains unquantified. Here, the authors reveal substantial microbial carbon fluxes across Greenland’s ice surface, in quantities that may s
Externí odkaz:
https://doaj.org/article/2ba5d9ce8e244a949088d073bdcfb63d
Autor:
J. M. Cook, A. J. Tedstone, C. Williamson, J. McCutcheon, A. J. Hodson, A. Dayal, M. Skiles, S. Hofer, R. Bryant, O. McAree, A. McGonigle, J. Ryan, A. M. Anesio, T. D. L. Irvine-Fynn, A. Hubbard, E. Hanna, M. Flanner, S. Mayanna, L. G. Benning, D. van As, M. Yallop, J. B. McQuaid, T. Gribbin, M. Tranter
Publikováno v:
The Cryosphere, Vol 14, Pp 309-330 (2020)
Melting of the Greenland Ice Sheet (GrIS) is the largest single contributor to eustatic sea level and is amplified by the growth of pigmented algae on the ice surface, which increases solar radiation absorption. This biological albedo-reducing effect
Externí odkaz:
https://doaj.org/article/f870750b981e47dfb6e844de2c42f2a2
Autor:
J. E. KAMINTZIS, J. P. P. JONES, T. D. L. IRVINE-FYNN, T. O. HOLT, P. BUNTING, S. J. A. JENNINGS, P. R. PORTER, B. HUBBARD
Publikováno v:
Journal of Glaciology, Vol 64, Pp 37-48 (2018)
The morphology of englacial drainage networks and their temporal evolution are poorly characterised, particularly within cold ice masses. At present, direct observations of englacial channels are restricted in both spatial and temporal resolution. Th
Externí odkaz:
https://doaj.org/article/8ed5ee462d494c4f860f7f4bb8cc34f0
Autor:
J. M. Cook, A. J. Hodson, A. S. Gardner, M. Flanner, A. J. Tedstone, C. Williamson, T. D. L. Irvine-Fynn, J. Nilsson, R. Bryant, M. Tranter
Publikováno v:
The Cryosphere, Vol 11, Pp 2611-2632 (2017)
The darkening effects of biological impurities on ice and snow have been recognised as a control on the surface energy balance of terrestrial snow, sea ice, glaciers and ice sheets. With a heightened interest in understanding the impacts of a chan
Externí odkaz:
https://doaj.org/article/081895f1a2e84badb19ad63799ff0a51
Autor:
G. Vatne, T. D. L. Irvine-Fynn
Publikováno v:
Hydrology and Earth System Sciences, Vol 20, Iss 7, Pp 2947-2964 (2016)
Despite an interest in the hydraulic functioning of supraglacial and englacial channels over the last 4 decades, the processes and forms of such ice-bounded streams have remained poorly documented. Recent glaciological research has demonstrated the p
Externí odkaz:
https://doaj.org/article/4ecf583133ea484ebed131eefe1ee1b2
Publikováno v:
Biogeosciences, Vol 11, Iss 19, Pp 5365-5380 (2014)
A cryoconite granule is a near-spherical aggregation of biota and abiotic particles found upon glacier surfaces. Recently, microstructural studies have revealed that photosynthetic microorganisms and extracellular polymeric substances (EPS) are omnip
Externí odkaz:
https://doaj.org/article/73a9bf3cf0e040c997334a7093fb7b5d
Publikováno v:
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXIX-B5, Pp 435-440 (2012)
Glaciers are sensitive to climatic variation and a particular developing area of investigation is in the field of "cryoconite”, referring to dustlike residues which form on the glacier surface. Cryoconite absorbs the Sun's shortwave energy, accele
Externí odkaz:
https://doaj.org/article/bbe6bce3f26745c0918ba2cbaf469521
Autor:
T D L, Irvine-Fynn, A, Edwards, S, Newton, H, Langford, S M, Rassner, J, Telling, A M, Anesio, A J, Hodson
Publikováno v:
Environmental microbiology. 14(11)
Uncertainty surrounds estimates of microbial cell and organic detritus fluxes from glacier surfaces. Here, we present the first enumeration of biological particles draining from a supraglacial catchment, on Midtre Lovénbreen (Svalbard) over 36 days.
Autor:
T. D. L. Irvine-Fynn, B. J. Moorman, I. C. Willis, D. B. Sjogren, A. J. Hodson, P. N. Mumford, F. S. A. Walter, J. L. M. Williams
Publikováno v:
Hydrological Processes; Jan2005, Vol. 19 Issue 1, p115-135, 21p