Zobrazeno 1 - 10
of 11
pro vyhledávání: '"G. J. Michaelson"'
Publikováno v:
SOIL, Vol 1, Iss 1, Pp 147-171 (2015)
Knowledge of soils in the permafrost region has advanced immensely in recent decades, despite the remoteness and inaccessibility of most of the region and the sampling limitations posed by the severe environment. These efforts significantly increased
Externí odkaz:
https://doaj.org/article/ee75a9d5ad9b44e1a7370b18e830d3c5
Autor:
G. Hugelius, J. Strauss, S. Zubrzycki, J. W. Harden, E. A. G. Schuur, C.-L. Ping, L. Schirrmeister, G. Grosse, G. J. Michaelson, C. D. Koven, J. A. O'Donnell, B. Elberling, U. Mishra, P. Camill, Z. Yu, J. Palmtag, P. Kuhry
Publikováno v:
Biogeosciences, Vol 11, Iss 23, Pp 6573-6593 (2014)
Soils and other unconsolidated deposits in the northern circumpolar permafrost region store large amounts of soil organic carbon (SOC). This SOC is potentially vulnerable to remobilization following soil warming and permafrost thaw, but SOC stock est
Externí odkaz:
https://doaj.org/article/6e79a164df5b43259ac6da9f81034661
Autor:
U Mishra, J D Jastrow, R Matamala, G Hugelius, C D Koven, J W Harden, C L Ping, G J Michaelson, Z Fan, R M Miller, A D McGuire, C Tarnocai, P Kuhry, W J Riley, K Schaefer, E A G Schuur, M T Jorgenson, L D Hinzman
Publikováno v:
Environmental Research Letters, Vol 8, Iss 3, p 035020 (2013)
The vast amount of organic carbon (OC) stored in soils of the northern circumpolar permafrost region is a potentially vulnerable component of the global carbon cycle. However, estimates of the quantity, decomposability, and combustibility of OC conta
Externí odkaz:
https://doaj.org/article/c2533a7eacd44aba9c59b93731c980da
Publikováno v:
Organic Geochemistry. 33:407-419
Soil organic matter (SOM) of five soil horizons from Arctic tundra and one soil horizon from a temperate region was separated into an extractable fraction (EF) and a non-extractable fraction (NEF) by dilute alkali. The modified classical fractionatio
Autor:
G. Hugelius, J. Strauss, S. Zubrzycki, J. W. Harden, E. A. G. Schuur, C. L. Ping, L. Schirrmeister, G. Grosse, G. J. Michaelson, C. D. Koven, J. A. O'Donnell, B. Elberling, U. Mishra, P. Camill, Z. Yu, J. Palmtag, P. Kuhry
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f9b672a9323431f5d43f027744370f79
https://doi.org/10.5194/bgd-11-4771-2014-supplement
https://doi.org/10.5194/bgd-11-4771-2014-supplement
Publikováno v:
Cryosols ISBN: 9783642058561
Soils of northern regions contain about 26% of the terrestrial C-stocks; the Arctic and boreal zones each hold about 12 to 13% (Post et al., 1982). Under the climatic conditions of the recent geological past, these regions have served as a sink for a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::09046a45feed5c93ff44a74586ad05bd
https://doi.org/10.1007/978-3-662-06429-0_23
https://doi.org/10.1007/978-3-662-06429-0_23
Publikováno v:
BMVC
We have been developing techniques for deriving parallel implementations of vision algorithms from prototypes written in a functional language (SML). Initially, we analysed simple, well understood algorithms to allow the prototyping methodology to be
Publikováno v:
Arctic and Alpine Research. 28:414
Tundra soil carbon stores ranged from a low of 16 kg C m-3 for a northern foothills ridge top site to a high of 94 kg C m-3 for a Barrow coastal plain tundra. Relatively low carbon stores were found in riparian shrubland, barren mountain slope, and a
Autor:
D. A. Walker, G. J. Jia, H. E. Epstein, M. K. Raynolds, F. S. Chapin III, C. Copass, L. D. Hinzman, J. A. Knudson, H. A. Maier, G. J. Michaelson, F. Nelson, C. L. Ping, V. E. Romanovsky, N. Shiklomanov
Publikováno v:
Permafrost & Periglacial Processes; Apr/Jun2003, Vol. 14 Issue 2, p103, 21p
Publikováno v:
Agronomy Journal. 74:694-699