SIMMER WORKSHOP (Science, Policy & Heat-Health Decision Making) Toronto

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Transcription:

SIMMER WORKSHOP (Science, Policy & Heat-Health Decision Making) Toronto Weather & Climate Modelling in Toronto & The Significant Results for Public Health October 24, 2013 Christopher Ll. Morgan, PhD Program Manager, Environment & Energy Office, City of Toronto

Address What is novel about the approach? How does the research help inform policies to reduce heat-related health impacts? How could this information feed into an integrated model? 2

Why Use a New Approach? To address our reservations with GCM / RCM Cell Areas Too Big (North Bay & Buffalo = same) No Great Lakes, Niagara Escarpment, ORM etc 30 Year Normal (latest available in 2006 = 1960-90 All About Means NOT our COSTLY EXTREMES To give us independence from the status quo Re: coasts, forests, agriculture, ice etc We (80%-90%) live in cities & need answers re cities To give us control over parameters considered We need answers re the extremes of heat & pptn. 3

New Questions. To Answer: New Questions Focused on obtaining data concerning: Future Extremes-of-Weather (e.g., Heat Waves & Torrential Storms) rather than Future Averages-of-Climate (e.g., Average Temperature & Average Rainfall) But examined such Averages to check model validity! 4

Three Intended Phases Phase 1 Examine What Happens Now and Why ie What Drives our Weather & Climate? Phase 2 Comparative Modelling Assessment for Toronto Best Models? Scales? Time Periods? Scenarios? Phase 3 Fully Model at Appropriate Scale & Time Period etc Consistency of Changes with Climate Drivers? 5

But. Following RFP Call With help from Science Advisors Group Realized the strongest Proposal -- also included part of Phase 2 So We Opted for a Phase 1+ Approach Would Still Like to do Phase 2 (ii) + Phase 3

New & Innovative Local Model Approach Global Climate Models + Regional Climate Models + Local Weather Model (1km 2 Cells) SENES Consultants ran the computer models ADVISORS & PEER REVIEW GROUP Environment Canada Ontario Ministry of the Environment Toronto Regional Conservation Authority Subsequently adopted by US National Centre for Atmospheric Research + MOE + UofT (W.R.Pelltier) 7

Major Components of New Approach Dynamic Downscaling from GCM/RCM to WRF WRF Weather Research Forecast Model 10 Year Period 2000-2009 & 2040-2049 1 km x 1 km grid scale A1B scenario 8

Future Weather Modelling Global Climate Model (GCM) output data was fed into the Hadley U.K. Met. Centre s Regional Climate Model (RCM / Precis) RCM output data was then fed into the Weather Forecast Model (WRF) for an area greater than the GTA but focusing on Toronto Used Future IPCC Scenario A1B with a moderate economic/political outlook and a likely future reality looked at extremes

New Approach & New Questions Included Local Influences (Great Lakes, Niagara Escarpment & Oak Ridges Moraine) Examined 10 Year Periods (not 30 Year Periods) Wanted to obtain data and information concerning the future extremes-of-weather rather than the future means-of-climate. Such as HEAT WAVES not just average annual or average summer temps.

Heat Wave. Definition A meteorological heat wave is defined by Environment Canada (Meteorological Service of Canada (MSC) - Ontario Region, 2009b). as. three or more consecutive days in which the maximum temperature is greater than or equal to 32 C.

Historical Data monitored 17 heat waves occurred in period 1971-2000 at Toronto Pearson International Airport Met. Stn. Average of 0.57 heat waves per year (17/30) The majority (65%) of heat waves lasted for the defining three days;. however, one heat wave lasted for 6 days, two heat waves lasted for 4 days, and three heat waves lasted for 5 days

Future. modelled: Heat Waves Looking at.. 2040-2049 We project 2.5 occurrences / year on average (>3 consecutive days w max. >= 32 C) Almost a 4.5x increase (from 0.57 to 2.5) Spatial Variation: 7.7 occurrences at Toronto Pearson, 4.4 occurrences at Etobicoke North 2.9 occurrences at the Don Valley East 0.2 occurrences at Scarborough

Future Temperature Differences Average annual temperatures increase by 4.4 o C BUT non-uniformly due to cooling influence of Lake Ontario, Simcoe etc

But.. Perhaps Examining Max Daily Temps together with High Overnight Temperatures (>24 C) could be more Valuable? We are currently extracting the relevant data (stay tuned but hopefully by Year End) Combinations of Heat Waves + SMOG Events Mostly spatially ubiquitous events But magnified in areas of Urban Canyons And other areas of poor urban street ventialtion 15

Future Warmer Temperatures Average annual temperatures increase by 4.4 o C Projected average winter temp. increases by 5.7 o C. Projected average summer temp. increases by 3.8 o C. The extreme daily minimum temperature - becomes less cold" by 13 o C. The extreme daily maximum temperature - "becomes warmer" by 7.6 o C.

Future Extreme Heat From 2000-2009 To 2040-2049 Mean Max. Daily Temperature 33 C 44 C Maximum daily air temperature is recorded at a weather station by selecting the highest 1-hourly air temperature within each period. (Averaged here over 10 years) Number of Days/Year > 30 C 20 66

Humidex From 2000-2009 to 2040-2049 Number of days Humidex >40 C eq 9 39 Maximum Humidex 48 C eq 57 C eq A Humidex above 45 is "dangerous When the humidex hits 54, heat stroke is imminent Note: Humidex remains within 10% of present for most of year but increases by 40% in February, and by 20% in July through to September (TEO Study)

Confidence in Results: Temperature Compared with Monitored Means (2000-2009) Toronto s Climate-Weather Model v.1= 8.70 o C EC s CRCM v.4.2.3 = 6.69 o C Monitored Data from Pearson = 8.73 o C Compared with Other Models (2040-2049) for GTA NB Compares High versus Low Resolution Models Our Delta 4.4 o C compares favourably with Low Res Models showing Deltas from -2.7 o C to 6.3 o C

Application of Results What the City wanted to obtain was data and information concerning the future extremes-of-weather rather than the future means-of-climate. Extremes are more significant for public operations, and both hard and soft service provision ranging from such basics as flood appropriate sewer & culvert pipe sizing, to heat wave appropriate load-bearing resistance of road surface materials, and. heat appropriate public services for the elderly and disadvantaged.

Application of Results What we see now re: Heat will get... MUCH WORSE!! Need Policy & Actions Need to Address & Adapt

ISSUE: Increased Summer Temperatures - A/C, Electricity Demand, Heat Vulnerability Expected in 2040-2049: Almost 6 times increase in A/C use during days with greater than 24 C 22

ISSUE: Increased Summer Temperatures Impact Air Quality (SMOG) Heat Waves & SMOG Events go hand in hand More Heat means More Smog 23

Heat & Smog Years [Jan 1 to Dec 31] # of SMOG Advisory Events # of SMOG Advisory Days 2003 5 12 2004 6 14 2005 14 48 2006 5 11 2007 11 29 2008 6 13 2009 2 4 2010 2 8 2011 1 1 2012 8 16 Total (2003-2012) 60 156 Average (2003-2012) 6 15.6 24

New Directions (3) 25 Adaptation (Urban Planning & Urban Design) Amend Provincial Policy Statement (PPS) -- done Include in City s Official Plan -- done Tool Kit for Planners (Urban Design) -- in progress Test & Develop Concepts Standard -- in future Develop Appropriate Designs & Configurations from 3-Dimensional AQ Modelling & Technical Analysis of Downtown Tall Buildings & Streets

Urban Canyon Problems 26

NOx Ann PM2.5 Ann 27

AQ in Downtown Canyons Today General Air Quality in Downtown Urban Canyon Areas of Toronto expressed as a percentage of Provincial Ambient Air Quality Criteria Percentages of AAQCs by Time Period Considered Air Quality Model Approaches Worst Case Day [Once a Year] Average Day [Year Long] Modelled Results as Verified Against Monitored Data of Toronto as a Featureless Plain NO BUILDINGS Modelled Results (same as above) but adapted using simple proportional land use coverage (GIS data) to better represent Complex Urban Terrain BUILDINGS INCLUDED 150% 75% 250% 125% 28

3D AQ Modelling - Computer + Physical 29

Buildings & Street Design 30

Air Flow Between & Through Buildings 31

How to Use Weather-Climate Data in an Integrated Model Use to address growth of future heat problems for all policies, actions etc to the same level of threat Allow subsequent completion of Phase 2 and Phase 3 to be incorporated into integrated model Ongoing monitoring of Temperature etc re: recent past & present coupled with comprehension of Climate Drivers to validate patterns of changes Provide feedback re needs from integrated model to inform future local weather-climate assessments 32

It will get much hotter more often! The End Questions and Answers Can Contact: cmorgan1@toronto.ca 416-392-6903