Zobrazeno 1 - 10
of 13
pro vyhledávání: '"W. R. Skinner"'
Publikováno v:
Annales Geophysicae, Vol 15, Pp 1089-1098 (1997)
The High Resolution Doppler Imager (HRDI) and the Wind Imaging Interferometer (WINDII) in- struments, which are both on the Upper Atmosphere Research Satellite, measure winds by sensing the Doppler shift in atmospheric emission features. Because
Externí odkaz:
https://doaj.org/article/425e85b804fb49d796e967c38bc09fd9
Publikováno v:
Climatic Change. 72:1-16
Historical relationships between weather, the Canadian fire weather index (FWI) system components and area burned in Canadian ecozones were analysed on a monthly basis in tandem with output from the Canadian and the Hadley Centre GCMs to project futu
Autor:
B. M. Wotton, E. M. Bosch, J. A. Mason, Mike D. Flannigan, J. B. Todd, Brian J. Stocks, David L. Martell, W. R. Skinner, K. A. Logan
Publikováno v:
Theoretical and Applied Climatology. 71:157-169
In Canada, the average annual area of burned forest has increased from around 1 million ha in the 1970’s to over 2.5 million ha in the 1990’s. A previous study has identified the link between anomalous mid-tropospheric circulation at 500 hPa over
Publikováno v:
Theoretical and Applied Climatology. 63:89-105
There is evidence that the area burned by wildland fire has increased in certain regions of Canada in recent decades. One cause for this increase is changes in the mid-tropospheric circulation at 500 hPa over northern North America. This study examin
Publikováno v:
Global Change Biology. 4:3-16
The North American mid-continent population of lesser snow geese (Anser caerulescens caerulescens) breeds in coastal areas of the Hudson Bay region. Breeding success is highly variable, particularly during recent decades. The availability of long-ter
Publikováno v:
Journal of Geophysical Research. 111
[1] Relationships between variations in peak Canadian forest fire season (JJA) severity and previous winter (DJF) global sea surface temperature (SST) variations are examined for the period 1953 to 1999. Coupled modes of variability between the seaso
Autor:
Scott Palo, J. M. Russell, E. Talaat, Pingping Rong, Cora E. Randall, G. Crowley, Janet U. Kozyra, G. Maris, Stanley C. Solomon, J. Yee, B. A. Emery, M. G. Mlynczak, W. R. Skinner, Larry J. Paxton, Xiaohua Fang, Rick J. Niciejewski, Qian Wu
Publikováno v:
Recurrent Magnetic Storms: Corotating Solar Wind Streams
High-speed solar wind streams originating from large coronal holes reached a maximum in 2003 during the descending phase of solar cycle 23. At the same time, magnetic activity (as indicated by the aa index) reached the highest levels of the last four
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ffb02276fe891d86fb6d3df51108b494
https://doi.org/10.1029/167gm24
https://doi.org/10.1029/167gm24
Autor:
J. A. Mason, W. R. Skinner, E. M. Bosch, J. B. Todd, David L. Martell, Mike D. Flannigan, K. A. Logan, Brian D. Amiro, Kelvin G. Hirsch, B. M. Wotton, Brian J. Stocks
Publikováno v:
Journal of Geophysical Research. 108
[1] A Large Fire Database (LFDB), which includes information on fire location, start date, final size, cause, and suppression action, has been developed for all fires larger than 200 ha in area for Canada for the 1959–1997 period. The LFDB represen
Publikováno v:
Advances in Global Change Research ISBN: 9789048153756
There is evidence that the area burned by wildland fire has increased in certain regions of Canada in recent decades. One cause for this increase is changes in the mid-tropospheric circulation at 500 hPa over northern North America. This study examin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::46a2adfaa64e62a3553f8ef9cd513aaa
https://doi.org/10.1007/0-306-47959-1_7
https://doi.org/10.1007/0-306-47959-1_7
Autor:
D. R. Bowes, W. R. Skinner
Publikováno v:
Geological Magazine. 106:477-484
SUMMARYThe field of composition and the geochemical trend of the lower portion of the stratiform Stillwater igneous complex correlate well with the field and trend for alpine-type ultrabasic masses in the nearby gneissic basement of the Beartooth Mou