Assessing Sensitivity to Changing Climate at High Latitudes Lee E. Penwell Amherst College Research...
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Transcript of Assessing Sensitivity to Changing Climate at High Latitudes Lee E. Penwell Amherst College Research...
![Page 1: Assessing Sensitivity to Changing Climate at High Latitudes Lee E. Penwell Amherst College Research and Discover Intern 2010 UNH Advisor: Richard Lammers.](https://reader036.fdocuments.in/reader036/viewer/2022062421/56649d145503460f949e85d4/html5/thumbnails/1.jpg)
Assessing Sensitivity to Changing Climate at High LatitudesLee E. PenwellAmherst CollegeResearch and Discover Intern 2010UNH Advisor: Richard Lammers
![Page 2: Assessing Sensitivity to Changing Climate at High Latitudes Lee E. Penwell Amherst College Research and Discover Intern 2010 UNH Advisor: Richard Lammers.](https://reader036.fdocuments.in/reader036/viewer/2022062421/56649d145503460f949e85d4/html5/thumbnails/2.jpg)
Project Objectives
•Identify areas most sensitive to climate change in the pan-Arctic
•Assess the uncertainty of future climate change in the pan-Arctic
•Assess the human impact
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Arctic Climate Change Index (ACCI)
•Based on F. Giorgi’s [2006] Regional Climate Change Index (RCCI)
•Future: 2080-2099, A2 (high range) and B1(low range) scenarios
•Present: 1960-1999, 20c3m scenario
•Two Seasons▫Cold – December, January, February▫Warm – June, July August
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Key Differences
• Finer Scale: Northern Hemisphere EASE Grids, 25.1 km x 25.1 km cells
• Calculated separately for each model and scenario
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Variables
•Warming amplification factor (WAF)Change in temperature relative to regional mean temperature change
•Change in temperature interannual variability (TSD) Calculated as standard deviation
•Change in precipitation (ΔP)
•Change in precipitation interannual variability (PCV) Calculated as coefficient of variation
![Page 6: Assessing Sensitivity to Changing Climate at High Latitudes Lee E. Penwell Amherst College Research and Discover Intern 2010 UNH Advisor: Richard Lammers.](https://reader036.fdocuments.in/reader036/viewer/2022062421/56649d145503460f949e85d4/html5/thumbnails/6.jpg)
Variable Reclassification
Values from Giorgi [2006]
Reclassification WAF (°C) TSD (%) P Δ (%) PCV (%)
0 < 1.1 < 5 < 5 < 5
1 1.1-1.3 5-10 5-10 5-10
2 1.3-1.5 10-15 10-15 10-20
4 > 1.5 > 15 > 15 > 20
![Page 7: Assessing Sensitivity to Changing Climate at High Latitudes Lee E. Penwell Amherst College Research and Discover Intern 2010 UNH Advisor: Richard Lammers.](https://reader036.fdocuments.in/reader036/viewer/2022062421/56649d145503460f949e85d4/html5/thumbnails/7.jpg)
Using the reclassified values:
ACCI =
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Warming Amplification Factor
CCCma CGCM3.1, SresB1, Cold Season
1.1 - 1.3
1.3 - 1.5
< 1.1
> 1.5
Precipitation Interannual Variability
Temperature Interannual Variability
Change in Mean Precipitation
< 5%
5 -10%
10 -15%
> 15%
< 5%
5 -10%
10 -15%
> 15%
< 5%
5 -10%
10-20%
> 20%
0
1
2
4
0
1
2
4
0
1
2
4
0
1
2
4
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Seasonal ACCI
0
1
2
3
4
5
6
7
8
9
10
11
12
13
14
16CCCma CGCM3.1, SresB1, Cold Season
ACCI Value
Least sensitive
Mostsensitive
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ACCI, 1 model, 1 scenario
CCCma CGCM3.1, SresB1
< 8
8 - 12
12 - 16
16 - 20
> 20
ACCI Class
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Limitations
•No assessment of March-May and September-November
•Reclassification can conceal variability
•Comparative Index
•Not adequately tested as a useful tool for policy decisions
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Mean ACCI, 8 models, 2 Scenarios
< 8
8 - 12
12 - 16
16 - 20
> 20
ACCI Class
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Highly Sensitive Regions
< 8
8 - 12
12 - 16
16 - 20
> 20
ACCI Class
Saskatchewan & S. Alberta
S. YeniseyNorth American High Latitudes
SW Alaska
Siberia
S. Ob’
European Russia
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Uncertainty [standard deviation of ACCI for all models and scenarios]
< 2
2 - 3
3 - 4
4 - 5
5 - 6
> 6
Standard Deviation
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Region Standard DeviationCertainty of High
Sensitivity
European RussiaLow for majority of highest ACCI class
Likely
North America High Latitudes
Low Likely
Saskatchewan & Southern Alberta
Variable Uncertain
SiberiaLow, especially for the highest ACCI class
Likely
Southern Ob’ Variable Uncertain
Southern Yenisey Low Likely
Southwestern Alaska VariableUncertain, especially for the highest ACCI class
Qualitatively Linking Uncertainty and ACCI
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Population
< 10
10 - 100
100 - 500
500 - 1,000
1,000 - 5,000
5,000 - 10,000
10,000 - 50,000
50,000 - 100,000
100,000 - 500,000
500,000 - 1,000,000
People/Grid Cell
Center for International Earth Science Information Network (CIESIN), Columbia University; and Centro Internacional de Agricultura Tropical (CIAT). 2005. Gridded Population of the World Version 3 (GPWv3): Population Grids.
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Linking Population, ACCI & Uncertainty
ACCI Classes Ranked By Uncertainty
Uncertainty: High Medium Low
< 8
8 - 12
12 - 16
16 - 20
> 20
ACCI Class
< 1%
4%
15%
31%
50%
Lowest Uncertainty Highest Population
% of Population in ACCI Class
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Concluding Remarks
•The ACCI identified areas sensitive to climate change in the pan-Arctic
•The most sensitive regions have a lower average uncertainty
•65% of the pan-Arctic population falls under the 2 highest ACCI classes
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NASA Connections
•Satellite climate monitoring should be aware of areas with high sensitivity and areas of uncertainty.
•Remote sensing can provide ongoing monitoring of ecosystems, urbanization and land use/land cover changes.
![Page 20: Assessing Sensitivity to Changing Climate at High Latitudes Lee E. Penwell Amherst College Research and Discover Intern 2010 UNH Advisor: Richard Lammers.](https://reader036.fdocuments.in/reader036/viewer/2022062421/56649d145503460f949e85d4/html5/thumbnails/20.jpg)
• Stanley Glidden, Water Systems Analysis Group• George Hurtt, Research & Discover Program• Laboratory for Remote Sensing and Spatial Analysis,
Complex Systems Research Center, University of New Hampshire
• National Science Foundation Office for Polar Programs• The Program for Climate Model Diagnosis and
Intercomparison and the World Climate Research Programme's Working Group on Coupled Modeling
Acknowledgments
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Pan-Arctic Permafrost
Continuous 90-100%
Discontinuous 50-90%
Isolated 0-10%
Sporadic 10-50%
Pan Arctic Outline
Permafrost Classification
International Permafrost Association (IPA)
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Land Cover
The Global Land Cover Facility (GLCF)
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Data• World Climate Research Programme's Coupled
Model Intercomparison Project phase 3 (CMIP3) multi-model dataset compiled for the Intergovernmental Panel on Climate Change
BCCR BCM2.0 CCCma CGCM3.1GFDL CM2.1 INM-CM3.0MIROC3.2 medres MPI ECHAM5 NCAR CCSM3.0 UKMO HadCM3
• Sres A2: low range emissions• Sres B1: high range emissions