1) The study quantifies the impact of greenhouse gas emissions, climate downscaling, and land-use change on urban heat stress scenarios in Belgium.
2) It reconstructs urban heat stress for 1979-2010 and projects future changes using a regional climate model under different greenhouse gas concentration scenarios and land use change projections.
3) The results indicate urban and semi-urban areas will experience greater increases in heat stress than rural areas due to synergistic effects of climate change, urban heat islands, and urban expansion.
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EGU2016_CORDEXBE
1. The impact of green-house gas emissions,
climate downscaling and land-use change
on Belgian urban heat stress scenarios
Hendrik Wouters, Nicole van Lipzig, Sam Vanden Broucke, Lien Poelmans, Hossein Tabari,
Parisa Hosseinzadeh Talaee, Johan Brouwers, Matthias Demuzere, Dirk Lauwaet, Bino Maiheu,
and Koen De Ridder
6. There were more than 400 additional deaths in
Belgium during heat wave in summer 2015
Belgian Scientific Institute of Public Health
=
~遜
7. Objectives
Hindcast for urban heat stress in Belgium
Projections
To quantify the different drivers future HS changes
8. Objectives
Hindcast for urban heat stress in Belgium
Projections
To quantify the different drivers future HS changes
9. min, max,18.2 29.6 ,i i i
i
HGD T C T C h
刻 逸 削 誌
Urban heat stress index
[De Ridder., et al 2015]
Heat-wave degree days [属C day]:
Heat wave day hi
Threshold-based index
12. COSMO-CLM
Scenarios Risk assessment
Land characteristics
GHG concentration
Boundary climate
High-resolution
3D climate statistics
GHG Emissions
Land-use change
Urban heat stress
Heavy precipitation and floods
Air pollution
Regional climate model [Rockel et al., 2008]Regional climate model
20. Objectives
Hindcast for urban heat stress in Belgium
Projections
To quantify the different drivers future HS changes
21. Objectives
Hindcast for urban heat stress in Belgium
Projections
To quantify the different drivers future HS changes
22. Impervious surface area [%]
Output from
Spatial model
[Engelen et al., 2011)]
Land use
change
23. Impervious surface area [%]
Land use
change
Business as usual
Output from
Spatial model
[Engelen et al., 2011)]
24. Delta change approach
[Tabari et al., 2014]
Changes in ensemble statistics are applied to the hindcast
RCP2.6, RCP4.5, RCP6.5 and RCP 8.5
11 GCM models, 31 simulations
Three ensemble scenarios:
GHG Emission
25. Delta change approach
(Tabari et al., 2014)
Offset applied on HISTorical record
RCP2.6, RCP4.5, RCP6.5 and RCP 8.5
11 GCM models, 31 simulations
Three scenarios:
Low
temperatures
High
temperatures
GHG Emission
60-year Changes in daily temperatures [属C]
1 2 3 4 5 6 7 8 9 10
0
1
2
3
4
5
bin
Apr may Jun Jul Aug Sep
0
1
2
3
4
5
HIGH
MEDIAN
LOW
Low
temperatures
High
temperatures
32. Future change heat stress: drivers
(Decomposition methodology: Stein and Alpert, 1993)
Urban
Semi-urban
Rural
Greenhouse gas-induced changes in climate statistics
Monthly mean temperature change
33. Future change heat stress: drivers
(Decomposition methodology: Stein and Alpert, 1993)
Urban
Semi-urban
Rural
Greenhouse gas-induced changes in climate statistics
Monthly-mean temperature change
Changes in temperature distribution
34. Future change heat stress: drivers
(Decomposition methodology: Stein and Alpert, 1993)
Urban
Semi-urban
Rural
Greenhouse gas-induced changes in climate statistics
Monthly-mean temperature change
Changes in temperature distribution
High-resolution climate downscaling
Monthly-mean
35. Future change heat stress: drivers
(Decomposition methodology: Stein and Alpert, 1993)
Urban
Semi-urban
Rural
Greenhouse gas-induced changes in climate statistics
Monthly-mean temperature change
Changes in temperature Distribution
High-resolution climate downscaling
Monthly-mean
Time dependency
36. Future change heat stress: drivers
(Decomposition methodology: Stein and Alpert, 1993)
Urban
Semi-urban
Rural
Greenhouse gas-induced changes in climate statistics
Monthly-mean temperature change
Changes in temperature Distribution
High-resolution climate downscaling
Monthly-mean
Time dependency
Land-use change
37. Future change heat stress: drivers
(Decomposition methodology: Stein and Alpert, 1993)
Urban
Semi-urban
Rural
Greenhouse gas-induced changes in climate statistics
Monthly-mean temperature change
Changes in temperature Distribution
High-resolution climate downscaling
Monthly-mean
Time dependency
Land-use change
Synergy temperature distribution change and downscaling
38. Future change heat stress: drivers
(Decomposition methodology: Stein and Alpert, 1993)
Urban
Semi-urban
Rural
Greenhouse gas-induced changes in climate statistics
Monthly-mean temperature change
Changes in temperature Distribution
High-resolution climate downscaling
Monthly-mean
Time dependency
Land-use change
Synergy temperature distribution and downscaling
39. Future change heat stress: drivers
(Decomposition methodology: Stein and Alpert, 1993)
Urban
Semi-urban
Rural
Greenhouse gas-induced changes in climate statistics
Monthly-mean temperature change
Changes in temperature Distribution
High-resolution climate downscaling
Monthly-mean
Time dependency
Land-use change
Synergy temperature distribution and downscaling
40. Future change heat stress: drivers
(Decomposition methodology: Stein and Alpert, 1993)
Urban
Semi-urban
Rural
Greenhouse gas-induced changes in climate statistics
Monthly-mean temperature change
Changes in temperature Distribution
High-resolution climate downscaling
Monthly-mean
Time dependency
Land-use change
Synergy temperature distribution and downscaling
GHG Emission
1 2 3 4 5 6 7 8 9 10
0
1
2
3
4
5
Low
temperatures
High
temperatures
Temperature change [属C]
41. Future change heat stress: drivers
(Decomposition methodology: Stein and Alpert, 1993)
Urban
Semi-urban
Rural
Greenhouse gas-induced changes in climate statistics
Monthly-mean temperature change
Changes in temperature Distribution
High-resolution climate downscaling
Monthly-mean
Time dependency
Land-use change
Synergy temperature distribution and downscaling
42. Wouters et al. (in preparation), Green-house gas induced excess heat waves, heat
islands and urban expansion comprise inordinate future heat stress at the mid-latitude.