Assessment of post-fire changes in land surface temperature and surface albedo, and their relation with fire-burn severity using multitemporal MODIS imagery

被引:64
作者
Veraverbeke, Sander [1 ,2 ]
Verstraeten, Willem W. [3 ,4 ]
Lhermitte, Stefaan [3 ,5 ]
Van de Kerchove, Ruben [1 ]
Goossens, Rudi [1 ]
机构
[1] Univ Ghent, Dept Geog, BE-9000 Ghent, Belgium
[2] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[3] Royal Netherlands Meteorol Inst, NL-3730 AE De Bilt, Netherlands
[4] Eindhoven Univ Technol, Fluid Dynam Dept, NL-5600 Eindhoven, Netherlands
[5] Univ la Serena, Ctr Estudios Avanzados Zonas Aridas, La Serena, Chile
基金
美国国家航空航天局;
关键词
climate; NDVI; remote sensing; satellite; 2007 PELOPONNESE WILDFIRES; TIME-SERIES; FOREST-FIRE; BOREAL FOREST; VEGETATION RECOVERY; NORTHERN AUSTRALIA; INTERIOR ALASKA; SATELLITE IMAGERY; TROPICAL SAVANNA; SPATIAL-PATTERNS;
D O I
10.1071/WF10075
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
This study evaluates the effects of the large 2007 Peloponnese (Greece) wildfires on changes in broadband surface albedo (a), daytime land surface temperature (LSTd) and night-time LST (LSTn) using a 2-year post-fire time series of Moderate Resolution Imaging Spectroradiometer satellite data. In addition, it assesses the potential of remotely sensed a and LST as indicators for fire-burn severity. Immediately after the fire event, mean a dropped up to 0.039 (standard deviation = 0.012) (P < 0.001), mean LSTd increased up to 8.4 (3.0) K (P < 0.001), and mean LSTn decreased up to -1.2 (1.5) K (P < 0.001) for high-severity plots (P < 0.001). After this initial alteration, fire-induced changes become clearly smaller and seasonality starts governing the a and LST time series. Compared with the fire-induced changes in a and LST, the post-fire NDVI drop was more persistent in time. This temporal constraint restricts the utility of remotely sensed a and LST as indicators for fire-burn severity. For the times when changes in a and LST were significant, the magnitude of changes was related to fire-burn severity, revealing the importance of vegetation as a regulator of land surface energy fluxes.
引用
收藏
页码:243 / 256
页数:14
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