David Barber

Climate Change
Prof. David G. Barber CRC, DP
Centre for Earth Observation Science
Faculty of Environment
1
Fifth Assessment Report
Tenure Track Faculty (13)
Research Faculty (8)
Adjunct Faculty (8)
Barber, David (CRC)
Dmitrenko, Igor
MacDonald, Robbie
Rysgaard, Soeren (CERC)
Galley, Ryan
Michel, Christine
Stern, Gary (DFO chair)
Lui, George
Ferguson, Steve
Lot Shafi
Lukovich,
Prinsenberg, Simon
Puyan Majobi
Jennifer
Loseto, Lisa
Mundy, C.J.
McCullough,
Miller, Lisa
Kuzyk Zou. Zou.
Greg
Hammill, Mike
Ehn, Jens. E.
Raddatz, Rick
Gosselin, Michel
Hanesiak, John
Hubert, Casey
Papakyriakou, Tim
Ogi, Masayo
Wang, Feiyue
Halden, Norman
23 MSc, 20 PhD, 15 PDF, 28 Tech/admin = 115 staff
Iacozza, John
The Observational Record - Global mean surface temperature
anomalies relative to the 1951-1980 climatology
Hansen et al. 2014
Global mean surface temperature anomalies relative to the
1951-1980 climatology
Hansen et al. 2006
Our addiction to fossil fuels:
•  1990 emission = 20 billion tons
•  2013 emission = 32 billion tons
•  Natural rate of increase = 0.0001 ppm/yr
•  2000 rate of increase = 2.5ppm/yr
•  2030 rate expectation = 5ppm/yr
Broecker, 2014
Our warming planet:
•  2013 tied with 2009 and 2006 for the seventh
warmest year since 1880.
•  With the exception of 1998, the 10 warmest
years in the 134-year record all have occurred
since 2000, with 2010 and 2005 ranking as the
warmest years on record
NASA GISS
Sea Ice – dynamic over many scales
2011
2012
8
Industrialization of the Arctic
9
The
Polar Vortex
Effect on our climate?
Warm ocean cold continent hypothesis
• Decrease in gradient between the
tropics and pole
• Slows eastward progression of
Robsby waves
• Leads to persistence at mid latitudes
• Increase potential for extreme
weather (droughts, floods, heatwaves,
coldspells)
Francis and Vavrus, 2012
Global Surface T°
Friday, April 25, 2014
7:32 am
Our Cold Winter
(Ogi et al. 2014)
Climate:
•  Change
•  Varability
Manitoba effects:
2.
1.
1.  Rising Permafrost Temperatures
2.  Thinning Ice
3.
3.  Forest Fires
5.
4.  Ecological Changes
4.
5.  Extreme Weather
6.  Less Soil Moisture
7.  Flooding
6.
7.
Source: gov.mb.ca
Increased Hydrological Cycle (now underway)
Source: IPCC, SPM05
Moderate increases in precipitation since 55
the mid-1990s have doubled average
runoff and caused more frequent flooding 53
in the Red River valley.
500
400
600
700
51
49
800
800
Precipita)on 10, 20, 30%
1996-2005 vs 1946-1995
(blue = decrease)
47
Hydrological forcing
of a recent trophic surge
in Lake Winnipeg
45
-117
55
-113
-109
-105
-101
-97
-93
-89
53
50
100
200
51
300
500
G.K. McCullough, et. al. 2012.
49
Runoff 300
100
50
50, 100, 200%
1996-2005 vs 1946-1995
(blue = decrease)
47
45
-117
10
-113
-109
-105
-101
-97
-93
-89
n initiated
the implige on the
on-Churchill
ies is to
ng and opure and busidivided into:
$ŝ“ĕëÓë¹ŝĨ
ájÓŝĜÇĜ
d to use
centers.
e of the
lved in the
drology. As
ability to
egional level
different record periods can contribute to some of the
variability. Trend analysis results, such as those presented
in Figure 5, are intended to develop an understanding on the direction and significance of historic climate
change and not to project the change into the future.
FIGURE 5: HISTORIC TRENDS FOR ANNUAL TEMPERATURE (TOP) AND
ANNUAL PRECIPITATION (BOTTOM) FOR ENTIRE PERIOD OF RECORD.
voluntary emission reduction objectives. Manitoba
Hydro’s GHG emissions are small. They represent only
1% of the emissions within a province that represents
Infrastructure
Energy
only 3%Manitoba’s
of national emissions.
Despite and
Manitoba
Hydro’s
demands
arepoint,
influenced
by
low emissions
starting
the corporation
has
achieved substantial further reductions and exceeded
•  Changes in temperature
its voluntary
commitments. While national electricity
•  Precipitation patterns
sector emissions
grew
•  Rising sea
levelsby 10 percent since 1990, Mani•  Extreme
weather events
toba Hydro
has achieved
an average long-term emissions reduction of 9 percent over the same time period
(Figure 2).
Manitoba Hydro Direct GHG
Emissions Reduction
FIGURE 2: MANITOBA HYDRO DIRECT GHG EMISSIONS
TORIC
YSIS
l relevant
acterize
conditions
rmation
g future
ature and
ydrologic
ar interest
analysis of
annual
30 years in
e series
Source: Manitoba Hydro Climate Change Report, 2012-13
9
Manitoba Hydro also estimates the GHG implications of
its major projects using life cycle analysis. All forms of
electrical generation, including renewable sources, have
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Possible Impacts of Climate Change on Agricultural Crops in Manitoba
Source: Natural Resources Canada, Climate Change Impacts and Adaptation: A Canadian Perspective.
Cost of Natural Disasters is already a key impact to our economies
Cost of Natural Disasters is already a key impact to our economies
Overwhelming evidence - yet…..
Source: IPCC, SPM05
Climate change is here and
we need to plan for it!