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7th Workshop on Forest Fire Management - EARSeL, European ...

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EFFECTS OF FIRE ON SURFACE ENERGY FLUXES IN A CENTRAL SPAIN<br />

MEDITERRANEAN FOREST. GROUND MEASUREMENTS AND SATELLITE<br />

MONITORING<br />

J.M. Sánchez 1<br />

1 Applied Physics Department, Un Castilla-La Mancha, Albacete, Spain<br />

juanmanuel.sanchez@uclm.es<br />

E. Rubio 1,2 , F. R. López-Serrano 3 , V. Caselles 4 & M.M. Bisquert 4<br />

2 Regi<strong>on</strong>al Development Institute, Un. Castilla-La Mancha, Albacete, Spain<br />

3 School of Agr<strong>on</strong>omy Engineering, Un. Castilla-La Mancha, Albacete, Spain<br />

4 Earth Physics and Thermodynamics Department, Un. Valencia, Burjassot, Spain<br />

Abstract: <strong>Forest</strong> fires are <strong>on</strong>e of the main agents involved in the change of<br />

structure and functi<strong>on</strong> of ecosystems. In this work we used a set of 5<br />

Landsat 5 Thematic Mapper (TM) images, of the years 2007-2008, covering<br />

an area of mediterranean forest and shrubs, affected by a fire in the summer<br />

of 2001. Two c<strong>on</strong>trol areas (n<strong>on</strong>-burned) were established, representative<br />

of the pre-fire c<strong>on</strong>diti<strong>on</strong>s in the burned areas. The simplified twosource<br />

model STSEB was applied to elaborate instantaneous energy flux<br />

maps, at the time of the satellite overpass. A Bowen stati<strong>on</strong> placed in the<br />

study site permitted a previous validati<strong>on</strong> of the results. Regarding the<br />

energy fluxes the most remarkable is the increase of more than 150 W m -2<br />

in sensible heat flux at instantaneous scale, and 40 W m -2 at daily scale,<br />

and the decrease of more than 250 W m -2 at instantaneous scale, and 60 W<br />

m -2 (2.1 mm/day) at daily scale, in actual evapotranspirati<strong>on</strong>, observed in<br />

the forested area. In the shrubs area, the fire effect is almost negligible<br />

after 6 years, since the vegetati<strong>on</strong> regenerates.<br />

1 - Introducti<strong>on</strong><br />

<strong>Forest</strong> fires are highly destructive for nature, affecting the landscape, the<br />

natural cicle of the vegetati<strong>on</strong>, and the structure and functi<strong>on</strong>ing of ecosystems.<br />

Bey<strong>on</strong>d that, they also provoke changes in the local and regi<strong>on</strong>al<br />

meteorology, and particularly in the surface energy fluxes regimen. There is<br />

an increasing c<strong>on</strong>cern am<strong>on</strong>g the scientific community about the effect of<br />

forest fires <strong>on</strong> climate change at this point (Randers<strong>on</strong> et al., 2006).<br />

Remote sensing techniques allow us to estimate surface energy fluxes over<br />

large areas. In the present work we use the Simplified Two-Source Energy<br />

Balance model (STSEB), developed by Sánchez et al., (2008a), applied to<br />

high resoluti<strong>on</strong> imagery obtained from Landsat 5 Thematic-Mapper (TM).<br />

The objective of this study is to quantify the effect of a forest fire in terms<br />

of net radiati<strong>on</strong>, and soil, sensible, and latent heat fluxes in two different<br />

ecosystems, mature pine forests and shrublands.<br />

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