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Published byEleanor Osmond Modified over 9 years ago
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THE STRUCTURE OF DROUGHT Ronald Stewart University of Manitoba
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A lot of nothing?
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To illustrate some aspects of drought's 'structure' (internal features) OBJECTIVE
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The Canadian Prairies
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Mackenzie Saskatchewan 400 500 600 700 850 925 1000 300 -2.0 -3.0 0 1.02.03.0 PRESSURE (hPa) FLUX (1011 kg/Pa/month) VERTICAL MOISTURE FLUX PROFILE Into the Prairies Out of the Prairies
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PDSI- Palmer Drought Severity Index SPI- Standardized Precipitation Index ---
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COMMON VIEW …
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Drought … Not Too Hot TemperaturePrecipitation Summers of 2000, 2001 and 2002
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PRECIPITATION-TEMPERATURE ANOMALY Agricultural Years (Sept-Aug) Edmonton
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Monthly temperature anomalies: agricultural region of the Prairies
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CLOUD AMOUNT
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2001 ___________ 900 km ____________
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WATER AND ENERGY CYCLING Many factors affect the cycling of water and energy during drought
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CANADIAN PRAIRIES 2002
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Climatology Low precipitation events: 52% of total Sub-drought 2002 Low precipitation events: 60% of total Daily Precipitation Amounts Low precipitation event: < 10 mm
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VIRGA Summer 2002 - Edmonton Precipitation Amount Reduction (%) -49 Precipitation (h) 123 Virga (h) 130
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Cold Lake 24 April 2003 Hail and rain 243% of monthly average accumulation Cold Lake 1-3 October 2005 Rain and snow 143% of monthly average accumulation PRECIPITATION RATE 45 dBZ maximum 20 dBZ maximum
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OCCURRENCE OF CALM CONDITIONS
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DUSTSTORMS 32 major dust storms in Saskatchewan in 2002
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CANADIAN PRAIRIES 2002 _________ 900 km ___________
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June 6-9, 2002
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Palmer Drought Severity Index (PDSI) for agricultural years with severe drought ___ 900 km __
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DROUGHT TYPES The sustained lack of precipitation can be linked with different 'types' A drought can go between 'types'
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Drought has spatial and temporal 'structure' One can think of it as being of various 'types' Understanding drought needs to consider such features SUMMARY
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