Climate Change in Cities: Observations, Impacts, and Solutions · Observations, Impacts, and...
Transcript of Climate Change in Cities: Observations, Impacts, and Solutions · Observations, Impacts, and...
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Climate Change in Cities: Observations, Impacts, and Solutions
Philip B. DuffyClimate Central, Inc.
climatecentral.org
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Enjoy your coffee!
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climatecentral.org
THIS TALK APPROVED FOR
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More about my favorite subject (me)
• Climate research since 1990
• Mostly computer modeling
• My mission: apply climate modeling to societal impacts of climate change
Basedon What?
My calculations
For a minute you had me worried.
I believe we are entering another ice age!
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Agriculture
Recreation Water availability
Extreme eventsAir quality
Human health
Societal impacts of climate change:The basis of policy decisions
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Societal-impacts studies need climate projections having:
o Fine resolutiono to provide regional-scale fidelity
o Reliable information on extremeso because these have disproportionate societal impacts
o Quantified uncertaintieso usually by analyzing a large family of simulations
It’s difficult impossible to make projectionshaving all these properties!
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Outline
o What you need to know about climatechange
o Importance of citieso Climate change in cities: urban heat islandso Impacts of climate change in citieso Solutionso Parting thoughts
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Outline
o What you need to know about climatechange
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“The balance of evidence
suggests a discernible
human influence on
global climate”
“There is new and
stronger evidence that
most of the warming
observed over the last
50 years is attributable
to human activities”
“This s*@# is real!”
“Most of the observed
increase in globally
averaged temperatures
since 1950 is very likely
[>90%] due to the observed
increase in anthropogenic
greenhouse gas
concentrations”
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Observed historical
warming:
Projected future
warming:
Why the spaghetti?
15 models x 3 emissions scenarios = 45 curves
Future warming could be large
Results from 15 models, each simulating 3 CO2 scenarios
10º Fahrenheit!
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Yearly total precipitation may increase or decrease…
• Increases projected in Northern US• Southwest will get drier• not sure about California
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…but extreme precipitation is increasing
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Outline
o Importance of cities
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Facts about cities
o 0.5% to 2% of Earth’s area (estimates vary)o 50% of global population.o > 400 cities with 1,000,000+ peopleo 20 “mega-cities” with 10,000,000+ peopleo 80% of global CO2 emissionso 75% of global energy consumptiono Particularly susceptible to some important impacts of climate change.
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Outline
o Climate change in cities: urban heat islands
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Urban heat island
• an urban region that is warmer than surrounding rural areas;• first identified in London, 1820;• affects surface temperatures more than air temperatures.
Urban myth: Urban heat islands are the cause of
observed increased in global temperatures.
Fact: Urban heat islands have contributed
negligibly to global temperature increases.
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What causes urban heat islands?
• dark surfaces• dry, non-porous surfaces• local generation of heat• night-time heat retention by heavy materials
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Areas with less vegetation are warmer
Landsat thermal image
NYC August 14, 2002
Vegetation density
NYC August 14, 2002
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Los Angeles is the mother of all heat islands
Source: NOAA
Globally-averaged warming: about 1º F during this period
Estimated added annual electricity cost $100M (LBNL Heat Island Group)
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Urban Heat Islands can be hard to find in meteorological observations
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Cities have temperature microclimates
Source: T. Peterson, J. Climate, 2003
Warm
areas
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Source: Brian Stone, Georgia Inst. Of Technology
Most Urban Heat Islands grow slowly, if at all
Difference in warming rate between US cities and
surrounding regions: 1951-2000
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Source: Brian Stone, Georgia Inst. Of Technology
Degrees per century!
US cities are warming faster than surrounding regions, but differences are small
Estimates of warming rate difference
between cities and rural areas
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Urban Heat Islands: Summary
• Cities tend to be warmer than surroundingregions, although areas of warmth are spotty.
• This difference is increasing very slowly in mostcities.
• Regardless, cities are warming along witheverywhere else.
• Reducing temperatures in cities would be good.• The Urban Heat Island phenomenon has not
contributed significantly to global temperatureincreases.
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Impacts of climate change in cities
• extreme heat and heat stress mortality• air quality• inundations from sea level rise• water scarcity
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Impacts of climate change in cities
• extreme heat and heat stress mortality
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Small increases in average temperature produce many more record highs
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Extreme heat event of July, 2006:
• 100+ people died
• 100,000 livestock died
• 1,000 PG&E transformers exploded
• …
Source: Woody
Whitlatch, PG&E
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Night-time
trends
Day-time
trends
Summertime warming is much faster at nightCalifornia shown here, but this is true nearly everywhere
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Daily mortality in Paris: 2003 vs. 1999-2002
Source: IPCC WGII
Daily temperature in Paris: 2003 vs. 1999-2002
2003 European heat event: ~35,000 people died
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Heat Stress Mortality
• Hard to quantify, because cause of death usually not obviously
related to heat.
• Mortality influenced by duration of heat event, and by night-
time temperatures.
• Affects very old and very young more than others.
• “Short-term mortality displacement” can be significant, or not.
• Acclimation to high temperatures reduces vulnerability.
• Projected increases partly offset by projected decreases in
mortality due to cold
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Heat Stress Mortality…
Affects very old and very young more than others.
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Days per year with
dangerous heat
index: now
Days per year with
dangerous heat
index: increase by
end of century
Source: N. Diffenbaugh
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Impacts of climate change in cities
• air quality
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• ozone
Climate change is expected to affect air pollution from:
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Ozone (O3) basics
• stratospheric O3 is good; ground-level O3 is bad:– causes respiratory illness– estimated annual mortality 21,000 (Europe)
• ground-level O3 forms when sunlight and chemical “precursors” are present.• Vehicles are the main human source of precursors.• Warm summer days have more O3 because of
– more sunlight– the reactions that form O3 go faster
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Source: Jacob & Winner, Atmosphere Environment (2009)
Probability that 8-hour
ozone concentrations
exceeds 80 ppb
threshold
Heat increases O3 concentrations
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Days per Year Conducive to Forming 1-hr Max Ozone > 90 ppb in Southern California.
Source: Abdullah Mahmud, Mary Tyree, Dan Cayan, Nehzat Motallebi, and Michael J. Kleeman, “Statistical Downscaling of
Climate Change Impacts on Ozone Concentrations in California”, Journal of Geophysical Research, submitted for publication, 2007.
Climate change tends to increase ground-level O3
Number of days per year favorable to forming daily 1-hr max
ozone of 90 ppb or more
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Climate change and Ozone: Summary
• Warming tends to increase ground-level ozone concentrations;
• This effect is modest and could be offset byregulations.
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Impacts of climate change in cities
• inundations from sea level rise
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Source: Cayan et al. (2006) Projecting Future Sea Level; report to the California Energy Commission
High sea levels will occur much more often
Projected hours per year with Delta water level above historical 99.99% level…
…And much below-normal atmospheric pressure
This assumes a 30 cm rise in mean sea level
(actual sea level rise could be much more)
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City populations and buildings are vulnerable to sea level rise
Source: Pacific Institute
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Impacts of climate change in cities
• water scarcity
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Our water supply depends on snow:
Source: D. Pierce, UCSD
March
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Courtesy Jay Lund, UCD Civil Engineering
Inflows into Central Valley with climate change
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Climate change reduces water deliveries in wet, dry, and normal years
Annual State Water Project water deliveries
Source: Vicuna et al, CEC Report, 2006.
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Outline
o Solutions
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Solutions: Urban Climate Modificationaka Heat Island Reduction
• What: Deliberate modification of urban climate to
minimize local warming and its impacts.
• Why: Easier, cheaper, faster than addressing global-
scale warming. Does not require international
cooperation!
• Co-benefits: Job creation, community building,
empowerment. Reduced energy use reduces global-
scale climate change.
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How? Trees and vegetation
• Provide shade, and cool via evaporation. Numerous
co-benefits.
Cost: Direct annual cost $15 - $65 per tree (US EPA).
Net cost may be negative.
• PS: Planting trees does not necessarily reduce
global-scale climate change!
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???Planting trees doesn’t help??????global warming???
• Increasing biomass helps, but is not
sustainable!
• Trees are dark, which tends to cause
warming.
• Planting trees where surfaces would be
light has net warming effect.
• Planting trees in the tropics helps.
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How? Green Roofs
Cool via evaporation. Numerous co-benefits.
Installation cost: $10 - $25 / sq. foot, vs. $5 - $10 for e.g.
composition. Annual maintenance cost $0.75 - $1.50 / sq. foot.
Life-cycle cost: lower than conventional roof, mainly thru
reduced energy use.
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How? Cool Roofs
Cool via reflecting sunlight and reduced emissivity.
Installation cost: zero to $0.20 more / sq. foot than
conventional.
Net cost: $0.50/yr less than conventional, per sq. foot,
due to reduced energy costs.
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How well does this work?
Temperature
reductions
Ozone
reductions
Source: H. Akbari, LBNL
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How? Cool Pavement
Cools by reflecting sunlight and/or
increasing evaporation.
Co-benefits: Permeable pavements
reduce stormwater runoff, reduce tire
noise, and give better traction.
Cost: varies.
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Effects of more reflective pavement
Temperature
reductions
Ozone
reductions
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Comprehensive “Climate Action Plan”, includes:
• measures to reduce congestion
• building energy use reductions
mandatory home energy audits
standards for insulation
appliance energy efficiency
cool roofs
etc.
• waste reduction and recycling
• adaptation measures, including preparation for
extreme heat events (?!?!)
• “community outreach and empowerment”
Example: Berkeley, Ca
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(SICCUHI)
September 21-23, 2009
Berkeley, California.
Organized by Lawrence Berkeley National Lab
To learn more:
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Parting Thoughts
o Climate change is produced primarily by activities in and related to cities.o The direct impacts of climate change on humans are concentrated in cities.o Deliberate modification of urban climate to reduce heating is feasible and effective.o Policies are needed to incentivize widespread adoption.
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“Congestion pricing”: Charges certain vehicle
types to drive in central city.
Intended to reduce congestion
Also reduced emissions of NOX by 8%, PM10
by 6%, and CO2 by 16%
Example: London, UK.
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What causes urban heat islands?Rank Place Population Land area (sq miles) Persons per sq mile Persons per sq meter Anthropogenic
heat (kWhr/m2day)
1 New York city, NY7,322,564 308.9 23,705 0.00853 2.3
2 Los Angeles city, CA 3,485,398 469.3 7,427 0.00267 0.72
3 Chicago city, IL 2,783,726 227.2 12,252 0.00441 1.19
4 Houston city, TX 1,630,553 539.9 3,020 0.00109 0.29
5 Philadelphia city, PA 1,585,577 135.1 11,736 0.00422 1.14
6 San Diego city, CA 1,110,549 324 3,428 0.00123 0.33
7 Detroit city, MI 1,027,974 138.7 7,411 0.00267 0.72
8 Dallas city, TX 1,006,877 342.4 2,941 0.00106 0.29
9 Phoenix city, AZ 983,403 419.9 2,342 0.00084 0.23
10 San Antonio city, TX 935,933 333 2,811 0.00101 0.27
11 San Jose city, CA 782,248 171.3 4,567 0.00164 0.44
12 Baltimore city, MD 736,014 80.8 9,109 0.00328 0.88
13 Indianapolis city, IN 731,327 361.7 2,022 0.00073 0.2
14 San Francisco city, CA 723,959 46.7 15,502 0.00558 1.5
15 Jacksonville city, FL 635,230 758.7 837 0.0003 0.08
16 Columbus city, OH 632,910 190.9 3,315 0.00119 0.32
17 Milwaukee city, WI 628,088 96.1 6,536 0.00235 0.63
18 Memphis city, TN 610,337 256 2,384 0.00086 0.23
19 Washington city, DC 606,900 61.4 9,884 0.00356 0.96
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Source: Brian Stone, Georgia Inst. Of Technology
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Heat Stress Mortality
This image shows the differences in day time land surface temperatures
collected in the two years by the Moderate Resolution Imaging
Spectroradiometer (MODIS) on NASA’s Terra satellite. A blanket of deep
red across southern and eastern France (left of image center) shows
where temperatures were 10 degrees Celsius (18 degrees Fahrenheit)
hotter this summer. White areas show where temperatures were similar,
and blue shows where temperatures were cooler in 2003 than 2001.
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Local generation of heat
• Estimated at 65 W/m2 to 1600 W/m2.• This is huge• affects local but not global temperatures.
Urban heat islands have not contributed significantly to global
temperature increases
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Impacts of climate change in cities
• increased energy demand (for cooling)
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Higher electricity demand on warm days
Source: Franco and Sanstad, Climatic Change (2008)
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Higher peak demand on warm days
Source: Franco and Sanstad, Climatic Change (2008)
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Maximum temperatures will increase(4 cities in Ca)
Source: Franco and Sanstad, Climatic Change (2008)
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Projected increases in average and peak electricity demand (CalISO region)