the seasonal dependency of the urban heat island of cities in belgium with cclm/tu

Post on 20-Jul-2015

97 Views

Category:

Environment

0 Downloads

Preview:

Click to see full reader

TRANSCRIPT

16/07/2014

The seasonal dependency of the

urban heat island of cities in Belgium with CCLM/TUHendrik Wouters, Matthias Demuzere, Koen De Ridder, Nicole van Lipzig Meteoclim 2014

16/07/2014 4© 2014, VITO NV

Urban expansion!

figure from Poelmans and Van Rompaey., 2009

16/07/2014 5© 2014, VITO NV

Urban expansion!

figure from Poelmans and Van Rompaey., 2009

16/07/2014 8© 2014, VITO NV

²

Trapped infrared radiation

sensible heat

stored

efficiently

by building

materials

atmosphere

sensible heat

atmosphere

Stored in ground

Very hot surface!!

Trapped solar radiation

Dry surface: no evaporation

Efficiënt conversion

16/07/2014 9© 2014, VITO NV

Excess

release

during the

night

Large heat

Storage

In buildings

atmosphere

Stored in ground

Hot Surface is cooling

sensible heat

atmosphere 1

16/07/2014 10© 2014, VITO NV

2. Human activity

16/07/2014 11© 2014, VITO NV

2. Human activity -> heat emission

Energy converted to heat -> emitted to the atmosphere! 2

16/07/2014 15© 2014, VITO NV

» 1. Which of the processes and contribute the most to the urban heat-island of cities in and around Belgium?

» 2. Is there a seasonal dependency?

Research questions

21

16/07/2014 17© 2014, VITO NV

How?

» We adapt the regional climate model CCLM to take account for

» by including the processes and

» Applicable for both summer as for winter

» as efficiënt as possible (cfr. Computational cost, needed input parameters)

21

16/07/2014 18© 2014, VITO NV

Regional climate model? 2 components.

Landoppervlakmodel

Atmospheric model

Sensible heat,

Evapo(transpi)ration,

Upward radiation

Drag on the wind

Temperature,

Precipitation,

Wind,

Downward radiation

16/07/2014 19© 2014, VITO NV

Regional climate model? 2 components.

Land-surface model

Atmospheric model

Wouters et al., (2012). Comprehensive parametrization of surface-layer transfer

coefficients for use in atmospheric numeric models. Boundary-layer Meteorology

Wouters et al., The impact of impervious water-storage parametrization

on urban climate modelling. Urban Climate (under revision)

21

Sensible heat,

Evapo(transpi)ration,

Upward radiation

Drag on the wind

Temperature,

Precipitation,

Wind,

Downward radiation

16/07/2014 20© 2014, VITO NV

Model configuration

Global weather forecasts from ECMWF

resolution:12.5 km

Regional climate model CCLM

resolution: 2.8 km

16/07/2014 21© 2014, VITO NV

Measurements urban heat island

» Antwerp

Antwerp

“Aren’t we a

bunch of

modelers?”

16/07/2014 22© 2014, VITO NV

Urban heat island of Antwerp

16/07/2014 23© 2014, VITO NV

Urban heat island of Antwerp

» Mid-summer

21/07/2012 -> 21/08/2012

» Mid-winter

21/01/2013 -> 21/02/2013

Uur van de dag

16/07/2014 24© 2014, VITO NV

Urban heat island of Antwerp

Uur van de dag

21

» Mid-summer

21/07/2012 -> 21/08/2012

» Mid-winter

21/01/2013 -> 21/02/2013

16/07/2014 25© 2014, VITO NV

Urban heat island of Antwerp

» Mid-summer

21/07/2012 -> 21/08/2012

» Mid-winter

21/01/2013 -> 21/02/2013

Uur van de dag

21

16/07/2014 26© 2014, VITO NV

Urban heat island of Antwerp

» Mid-summer

21/07/2012 -> 21/08/2012

» Mid-winter

21/01/2013 -> 21/02/2013

Uur van de dag

21

16/07/2014 27© 2014, VITO NV

Effect of heat emission in the city?

» Mid-summer

21/07/2012 -> 21/08/2012

» Mid-winter

21/01/2013 -> 21/02/2013

Uur van de dag

21

16/07/2014 28© 2014, VITO NV

Effect of heat emission in the city?

» Mid-zomer

21/07/2012 -> 21/08/2012

» Mid-winter

21/01/2013 -> 21/02/2013

Uur van de dag

16/07/2014 29© 2014, VITO NV

Effect heat emission in the city?

» Mid-zomer

21/07/2012 -> 21/08/2012

» Mid-winter

21/01/2013 -> 21/02/2013

Uur van de dag

16/07/2014 30© 2014, VITO NV

geen stedelijke opbouw

anthropogene warmte

mid-summer

midnight

(averaged)

21 21

21

16/07/2014 31© 2014, VITO NV

mid-summer

midnight

(averaged)

21 21

2121

16/07/2014 32© 2014, VITO NV

mid-summer

midnight

(averaged)

21 21

2121

21

21

16/07/2014 33© 2014, VITO NV

mid-summer

midnight

(averaged)

21 21

2121

21

21

16/07/2014 34© 2014, VITO NV

mid-summer

midnight

(averaged)

21 21

2121

21

21 21

16/07/2014 35© 2014, VITO NV

stedelijke opbouw energieverspilling interactie

mid-summer

midnight

21 21 21

16/07/2014 36© 2014, VITO NV

+ +

=

totale impact

mid-summer

midnight

21 21 21

21

urban structure interactionenergy waste

16/07/2014 37© 2014, VITO NV

+ +

=

totale impact

Values for Brussels

1.97°C 0.68°C -0.21°C

2.44°C

mid-summer

midnight

21 21 21

21

urban structure interactionenergy waste

16/07/2014 38© 2014, VITO NV

+ +

=

total impact

Values for Brussels

+0.41°C +1.20°C +0.25°C

+1.97°C

mid-winter

midnight

21 21 21

21

urban structure interactionenergy waste

16/07/2014 39© 2014, VITO NV

Conclusions

» Both , as well as their determine the urban heat-island intensity of cities in Belgium, and their respective contributionsstrongly depend on the season

» Both positive as negative influences on the urban thermal comfort needsto be accounted for with regard to:

» Tempering urban heat during heat waves, versus cold waves

» Climate change (e.g. , …)

» (urban) land-use change

21 21

16/07/2014 40© 2014, VITO NV

Thank you for your attention!

livable

smart

cities

top related