CHANGING SUMMER CLIMATE ON THE PRAIRIES: FROM DROUGHTS TO FLOODS AN ASSESSMENT OF THE CAUSES AND CONSEQUENCES SINCE 1990

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CHANGING SUMMER CLIMATE ON THE PRAIRIES: FROM DROUGHTS TO FLOODS AN ASSESSMENT OF THE CAUSES AND CONSEQUENCES SINCE 1990 Ray Garnett Agro Climatic Consulting (ACC) Natural Resources Institute (NRI) The Extremes Workshop Inn at the Forks Winnipeg, Manitoba Tuesday, February 8, 2011.

INTRODUCTION The purpose of this talk is to present a preliminary assessment of the causes and consequences of extremely wet and dry May- Julys periods over the prairies since 1990 with special reference to 2010. Using rainfall data for the period 1950-2010 there have been six extremely wet (2010, 1991, 1999, 1993, 2005 and 2004) and two extremely dry (2009 and 2003) May-July periods since 1990. The summers of 2010, 1991, 1999, 1993, 2005, 2004, 2009 and 2003, are analyzed on a case-by-case basis in relation significant seasonal influences. Garnett et al. 2006 found that a combination of low (high) sunspot, a westerly (easterly) phase of the quasi-biennial wind oscillation, El Nino (La Nina) conditions and below (above) normal North American snow cover can act synergistically to produce a wet (dry) summers over the prairie region. Solar cycle 24 (2010-2021) will be compared and contrasted with the Dalton Minimum of 1795-1823.

STUDY AREA AND DATA SOURCES MONTHLY DATA FOR THE PERIOD 1950-2004 Precipitation and temperature for 51 stations Environment Canada Precipitation 2005-2010 for 30 stations Environment Canada Sunspot U.S. NOAA Geophysical Data Centre Boulder, Colorado. 30 hpa Quasi-Biennial Wind Oscillation (QBO) U.S. Climate Prediction Centre Nino 3 and Nino 3.4 sea surface temperatures U.S. Climate Prediction Centre North American snow (NAS) cover extent 1974-2004 U.S. Climate prediction Centre

PRECIPITATION AND TEMPERATURE OVER THE PRAIRIE REGION APRIL THROUGH SEPTEMBER OF 2010 Table 1. Precipitation (mm) Temperature (ºC) Actual Normal % of normal Actual Normal DFN April 54 27 200 6.4 3.6 + 2.8 May 95 47 202 9.2 10.8-1.6 June 102 74 138 15.2 15.4-0.3 July 71 67 106 19.7 18.0-0.6 August 74 55 134 16.7 17.0-0.7 September 54 41 132 10.1 11.2-1.1 Mean anomaly April-September 152-0.25 Note: Precipitation and temperatures are based on 30 and 10 stations respectively Normal amounts based on 100 stations for the period 1950-1995 WETTEST AND DRIEST MAY-JULYS FOR THE PERIOD 1950-2010 Extremely wet and dry years since 1990 highlighted Table 2. Wettest (mm/mo) Driest (mm/mo) 2010 88.3 1967 28.7 1991 85.5 1958 37.9 1999 84.4 1961 40.1 1993 82.5 1985 42.8 1953 82.1 2009 46.0 2005 81.0 1957 46.3 1986 77.3 2003 46.5 1977 77.1 1963 76.8 1965 76.7 2004 76.1 Mean 62.9 mm/mo 1 S.D. is 12.5 > 1 S.D 75.4 < 1 S.D 50.4

Svensmark and Calder 2007. The Chilling Stars: A New Theory of Climate Change.

Fig. 1. Sunspots per month for two wettest May-Julys Fig. 2. Accumulated Nino 3.4 sea surface temperatures before and during June-July of the two wettest May-Julys Working Hypothesis re: causes of two wettest May-Julys for the period 1990-2010 2010: Low sunspot activity, El Nino and below normal April NAS 1991: El Nino, westerly QBO, and below normal April NAS

Fig. 3. Sunspots per month before and during third and fourth wettest Fig. 4. Accumulated Nino 3.4 sea surface temperatures before and during June-July of third and fourth wettest Working Hypotheses re: causes of third and fourth wettest May-Julys 1999: Sunspots mostly favourable, below normal NAS in April 1993: Sunspots mostly favourable, El Nino, westerly QBO, below normal NAS

Fig. 5. Sunspots per month before and during fifth and sixth wettest Fig. 6. Accumulated Nino 3.4 sea surface temperatures before and during June and July of the fifth and sixth May-Julys Working Hypothesis re: causes of fifth and sixth wettest May-Julys during 1990-2010. 2005: Low sunspot activity, El Nino, westerly QBO Sept.-Dec., below normal Apr. NAS. 2004: Low sunspot activity, El Nino, below normal Apr. NAS

Fig. 7. Sunspots per month for two driest May-Julys Fig. 8. Accumulated Nino 3.4 sea surface temperatures before and during June-July of the two driest May-Julys Working Hypothesis re: causes for two driest May-Julys for the period 1990-2010 2003: Above average sunspot activity Sep-Aug, easterly QBO Dec-Jan 2009: La Nina conditions Dec-Mar (extremely late harvest, near record yields)

Table 1. Correlation coefficients of sunspots per month vs. PDSI values Station May June July May-July Data period N Brandon -0.077-0.119-0.091-0.104 1895-2001 107 Calgary -0.094-0.095-0.098-0.103 1895-2001 107 Coronation -0.207-0.183-0.141-0.183 1945-2001 57 Dauphin 0.030 0.040 0.073 0.051 1911-2001 91 Edson -0.019 0.024 0.027 0.012 1920-2001 82 Edmonton -0.132-0.249* -0.126-0.189 1916-2001 86 Estevan -0.278* -0.299* -0.259* -0.289* 1944-2001 58 Medicine Hat -0.192* -0.186-0.190-0.195* 1896-2001 106 Prince Albert -0.188-0.207* -0.252* -0.230* 1895-2001 107 Regina -0.180-0.247** -0.269*** -0.245** 1898-2001 104 Saskatoon -0.141-0.159-0.179-0.171 1902-2001 100 Swift Current -0.217* -0.179-0.212* -0.214* 1895-2001 107 Winnipeg -0.123-0.094-0.121-0.127 1895-2001 107 *Significant at the 5% level (two tailed) ** Significant at the 1% level *** Significant at the.1% level Based on June-Aug PDSI data 1913-2005 & (May-July precipitation 2005-2010) Currently in year 16 of the Hale Magnetic or 22-year Double Sunspot cycle Table 2. Drought and Flood Frequency during five Hale cycles since 1913 Polarity Year in Cycle Droughts (PDSI>-2.22) Floods (PDSI > 1.36) 1 1996 2 1955 3 4 1937 5 1938 1980 Positive 6 1918 2001 1939 7 1919 1940 8 1920 1961 1941 9 10 1943 11 12 1965 13 1988 1966 14 (2009) 15 1927 (2010) Negative 16 1949 1991 1928 17 1970 18 1930 1951 1993 19 1931 20 21 1974 1954 22 1975

Courtesy of Dr. M. L. Khandekar, and J Aleo

CONCLUSIONS * Since 1990 there have three times as many extremely wet May-Julys as extremely dry May-Julys. * Results Extremely wet May-Julys Sunspots QBO ENSO NAS 2010 F F F 1991 F F F 1999 F F 1993 F F F 2005 F F F F 2004 F F F Extremely dry May-Julys 2009 F 2003 F F *Significant correlations have been found between sunspot and PDSI data over the prairie region supporting the findings of Garnett et al 2006. *Observational evidence suggests we are now in second half of the Hale Cycle when there has been about three times as many extremely wet May-Julys as dry May-Julys for the period 1913-2010. *Some solar models predict the Sun could be entering a period like the Dalton Minimum at the time of Manitoba s Selkirk Settlers. A sunspot peak of no more than 50 sunspots per month around 2013-2014 would serve to confirm this.