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1. |
Drought as a natural disaster |
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Atmosphere-Ocean,
Volume 33,
Issue 2,
1995,
Page 195-222
J. Maybank,
B. Bonsai,
K. Jones,
R. Lawford,
E.G. O'Brien,
E.A. Ripley,
E. Wheaton,
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摘要:
Droughts are major natural disasters for many parts of the world. Dry areas, where the precipitation pattern is markedly seasonal, or is otherwise highly variable, are the most susceptible. The Canadian Prairies, together with the U.S. Great Plains, are one such area. While immediate loss of life is seldom a feature of most droughts, malnutrition and even starvation do follow severe droughts in some parts of the world. In Canada, economic losses, particularly in the agricultural sector, may reach several hundred millions of dollars in a drought year, with major socio‐economic repercussions affecting the entire region. Environmental damages include soil degradation and erosion, vegetation damage, slough and lake deterioration and wildlife loss. Unlike most other natural disasters, drought onset is difficult to identify. Droughts develop slowly, and until human activity begins to be affected by an on‐going reduction of precipitation, their existence is unrecognized. Development and application of specific soil moisture and drought indices based on cumulative precipitation deficits have enhanced drought monitoring programs. These in turn provide guidance on the need for mitigative measures that can be initiated early in the course of a drought. Any improvement in the timely application of these measures is, however, strongly dependent on being able to determine the drought's course, extent and likely severity at the earliest stage possible. The identification of precursor conditions for past drought has raised the possibility that the likelihood of a drought occurring in a particular year or growing season might be predictable. Teleconnections between North American precipitation patterns and ENSO events and other surface boundary conditions in the North Pacific have been detected. Forecasting seasonal temperature and perhaps precipitation anomalies appears to be potentially feasible using a suitable merging of precursor parameters and modelling methodologies. Clearly, future research must focus both on those precursors that have been identified and on a search for possible new ones. Development of better forecasting methodology is also essential. Research activity to identify and evaluate new mitigative measures should also be increased to keep pace with the prospects of drought predictability.
ISSN:0705-5900
DOI:10.1080/07055900.1995.9649532
出版商:Taylor & Francis Group
年代:1995
数据来源: Taylor
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2. |
Winter storms over Canada |
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Atmosphere-Ocean,
Volume 33,
Issue 2,
1995,
Page 223-247
R.E. Stewart,
D. Bachand,
R.R. Dunkley,
A.C. Giles,
B. Lawson,
L. Legal,
S.T. Miller,
B.P. Murphy,
M.N. Parker,
B.J. Paruk,
M.K. Yau,
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摘要:
Various type of winter storms occur over Canada and produce major impacts on society. Canada is subjected to extra‐tropical cyclones with all their embedded structures, as well as blizzards, mountain‐induced storms, lake effect storms and polar lows. Many of these storms are accompanied by heavy precipitation in the form of snow or freezing precipitation, bitterly cold conditions, strong winds, and blowing snow. The occurrence and nature of these storms are discussed in this review article.
ISSN:0705-5900
DOI:10.1080/07055900.1995.9649533
出版商:Taylor & Francis Group
年代:1995
数据来源: Taylor
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3. |
Recent progress in the operational forecasting of summer severe weather |
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Atmosphere-Ocean,
Volume 33,
Issue 2,
1995,
Page 249-302
Paul Joe,
Cliff Crozier,
Norman Donaldson,
Dave Etkin,
Erik Brun,
Steve Clodman,
Jim Abraham,
Stan Siok,
Henri‐Paul Biron,
Mike Leduc,
Phil Chadwick,
Steve Knott,
Jamie Archibald,
Glenn Vickers,
Steve Blackwell,
Rick Drouillard,
Alan Whitman,
Harold Brooks,
Nick Kouwen,
Richard Verret,
Gilles Fournier,
Bob Kochtubajda,
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摘要:
Summer severe weather (SSW) can strike suddenly and unexpectedly with disastrous consequences for human activity. Considerable progress has been made in the past ten years in the operational forecasting of SSW. Traditionally, SSW was defined to consist of tornadoes, strong winds, hail, lightning and heavy rain. Hazardous types of strong winds have recently been expanded to include microbursts, macrobursts and surfacing rear inflow jet damage behind mesoscale convective systems. Doppler radar was used to relate surface damage to the appropriate atmospheric phenomena, first diagnostically and then prognostically. This improvement in classification has fedback to and improved the forecast process. Concurrent progress has been made in the use of synoptic observations. The concept of helical wind profiles and improved knowledge of the role of dry mid‐level air has improved the forecasting of tornadoes and strong gusty winds. Moisture flux convergence, derived from surface measurements, shows great promise in identifying areas of storm initiation. Satellite imagery has been used to identify dynamical atmospheric boundaries. Numerical modelling of the interaction of environmental wind profiles and individual thunderstorms has greatly contributed to the understanding of SSW. Studies of spatial and temporal patterns of lightning, both specific cases and climatology, contribute to the forecasting of severe storms. Polarization radar results have shown progress in separating the signals of hail from those of rain and in the improved measurement of heavy rainfalls. Radar observation of clear air boundaries and their interactions show potential for the forecasting of thunderstorm initiation. Though not traditionally considered part of SSW, hurricanes that evolve into extra‐tropical storms share many of the same hazardous features. The progress in computing, communications and display technologies has also made substantial contributions to operational forecasting and to the dissemination of weather warnings.
ISSN:0705-5900
DOI:10.1080/07055900.1995.9649534
出版商:Taylor & Francis Group
年代:1995
数据来源: Taylor
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4. |
Hydrometeorological aspects of flood hazards in Canada |
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Atmosphere-Ocean,
Volume 33,
Issue 2,
1995,
Page 303-328
R.G. Lawford,
T.D. Prowse,
W.D. Hogg,
A.A. Warkentin,
P.J. Pilon,
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摘要:
Floods are major natural disasters in Canada and worldwide. Although technology has reduced the flood hazard in many areas, the world death toll from floods in recent decades still has averaged 4680 per year. During the summer of 1993, flooding in the U.S.A. caused an estimated $12 billion damage. These statistics confirm that floods are a major natural disaster.
ISSN:0705-5900
DOI:10.1080/07055900.1995.9649535
出版商:Taylor & Francis Group
年代:1995
数据来源: Taylor
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5. |
Storm waves in Canadian waters: A major marine hazard |
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Atmosphere-Ocean,
Volume 33,
Issue 2,
1995,
Page 329-357
MadhavL. Khandekar,
ValR. Swail,
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摘要:
In this paper, an overview of storm waves associated with intense weather systems affecting the east and west coasts of Canada is presented. The paper presents the wave climatology of the east and west coasts in terms of the 100‐year significant and maximum wave heights and further analyses the directional distribution of wave heights at selected locations in the Canadian east and west coasts offshore. The paper also analyses wave hazards associated with storm waves in the Beaufort Sea as well as the Canadian Great Lakes region. A section on ocean wave modelling provides a brief history of the development of ocean surface wave models and its present status. The paper further considers the impact of climate change scenarios on wave hazards and finally examines mitigation measures in terms of wave products available from operational wave models and related wave climatology.
ISSN:0705-5900
DOI:10.1080/07055900.1995.9649536
出版商:Taylor & Francis Group
年代:1995
数据来源: Taylor
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6. |
Storm surges in Canadian waters |
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Atmosphere-Ocean,
Volume 33,
Issue 2,
1995,
Page 359-387
T.S. Murty,
S. Venkatesh,
M.B. Danard,
M.I El‐Sabh,
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摘要:
Storm surges in various Canadian waters are reviewed. Following a brief discussion of the weather systems that cause storm surges in Canadian coastal and inland waters, the mathematical formulations to describe the development of storm surges are given. In reviewing storm surges in the different Canadian waters, particular attention is given to describe the influence of the presence of sea ice on surge development and the impact of shallow coastal areas, where the coastline configuration is itself changed by the surge, on inland penetration of the storm surge. The Canadian waters that may be affected by storm surges include the east and west coasts, the Beaufort Sea, the Gulf of St. Lawrence and the St. Lawrence estuary, Hudson Bay and the Great Lakes.
ISSN:0705-5900
DOI:10.1080/07055900.1995.9649537
出版商:Taylor & Francis Group
年代:1995
数据来源: Taylor
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