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Fourth Study Conference on BALTEX Scala Cinema Gudhjem

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Validati<strong>on</strong> of Boundary Layer Parameters and Extensi<strong>on</strong> of Boundary<br />

C<strong>on</strong>diti<strong>on</strong>s of the Climate Model REMO – Estimati<strong>on</strong> of Leaf Area Index<br />

from NOAA-AVHRR-Data<br />

Birgit Streckenbach und Eberhard Reimer<br />

Institute of Meteorology, Free University of Berlin, Carl-Heinrich-Becker-Weg 6-10, streckba@zedat.fu-berlin.de<br />

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

At this time the climate model REMO of the Max-Planck-<br />

Institute Hamburg works with fixed regi<strong>on</strong>al vegetati<strong>on</strong><br />

parameters for every m<strong>on</strong>th of the year. To obtain a better<br />

adaptati<strong>on</strong> to real c<strong>on</strong>diti<strong>on</strong>s the estimati<strong>on</strong> of the annual<br />

changes in vegetati<strong>on</strong>, especially deciduous forests, which<br />

significantly influence the boundary layer processes and in<br />

particular the moisture budget, is necessary. The Leaf Area<br />

Index (LAI) is a characteristic indicator for the type of<br />

vegetati<strong>on</strong> and its activity.<br />

2. Data and Method<br />

At the Institute of Meteorology of the Free University Berlin<br />

NOAA-AVHRR data for the European regi<strong>on</strong> are available<br />

day by day since 1989. The data are corrected to eliminate<br />

typical errors referring to calibrati<strong>on</strong> and shift in observati<strong>on</strong><br />

time. They are also adjusted to geographic coordinates and<br />

to a land mask.<br />

On the basis of these data from 1995 until 2002 during the<br />

vegetati<strong>on</strong> period (April-September) the LAI in the Baltic<br />

regi<strong>on</strong> was predicted pixelwise from the Normalized<br />

Difference Vegetati<strong>on</strong> Index (NDVI) for 1km x 1km resoluti<strong>on</strong><br />

using an algorithm from Sellers et al. (1996).<br />

At first 10 day composites of the NDVI were created to<br />

eliminate the disturbing influence of cloudiness. Missing or<br />

incorrect pixels were completed in time by harm<strong>on</strong>ic<br />

analysis and regi<strong>on</strong>ally by pixel neighbourhood rec<strong>on</strong>structi<strong>on</strong>.<br />

From these NDVI values the Fracti<strong>on</strong> of Absorbed<br />

Photosynthetic Active Radiati<strong>on</strong> (FAPAR) was predicted<br />

and then the LAI was determined using a modified USGS<br />

land cover classificati<strong>on</strong>. Finally the 1km x 1km, 10 day<br />

averaged LAI data were c<strong>on</strong>verted into the 1/6 degree<br />

resoluti<strong>on</strong> of the REMO climate model.<br />

3. Results<br />

In Figures 1 and 2 the Normalized Difference Vegetati<strong>on</strong><br />

Index and the Leaf Area Index are shown for the sec<strong>on</strong>d<br />

decade of June 2000 in the Western part of the <strong>BALTEX</strong><br />

regi<strong>on</strong>, derived from NOAA-AVHRR data. with a resoluti<strong>on</strong><br />

of 1km x 1km.The regi<strong>on</strong>al variability of the NDVI values is<br />

not very str<strong>on</strong>g.. In difference the LAI shows very high<br />

values in the Southern parts of Scandinavia and in the Alps<br />

regi<strong>on</strong>. The landuse in these regi<strong>on</strong> is characterised by<br />

agriculture, grassland and deciduous forests. This figure is a<br />

good example for the LAI as indicator for the activity of<br />

vegetati<strong>on</strong> and biomass producti<strong>on</strong>. For the detecti<strong>on</strong> of the<br />

interannual LAI development and its changes from year to<br />

year in dependence of the weather c<strong>on</strong>diti<strong>on</strong>s LAI data sets<br />

over a period of seven years for the whole <strong>BALTEX</strong> regi<strong>on</strong><br />

were created. They allow to make statistical evaluati<strong>on</strong> and<br />

to test the sensitvity of the REMO model against varying<br />

vegetati<strong>on</strong> parameters. To validate the used land cover<br />

classificati<strong>on</strong> ASTER and Landsat7 scenes with a resoluti<strong>on</strong><br />

of 250m up to 15m for single days were evaluated and<br />

compared with the NOAA data sets (DBS GmbH Mohnen).<br />

Figure 1. High resoluti<strong>on</strong> NDVI for the Western part of<br />

the <strong>BALTEX</strong> regi<strong>on</strong> (June 2000)<br />

Figure 2. High resoluti<strong>on</strong> LAI for the Western part of the<br />

<strong>BALTEX</strong> regi<strong>on</strong> (June 2000)<br />

References<br />

Sellers, P.J., Los, S.O., Tucker, C.J., Justice, C.O.,<br />

Dazlich, D.A., Collatz, G.J. and D.A. Randall, A<br />

revised land surface parameterizati<strong>on</strong> (SiB2) for<br />

atmospheric GCMs. Part II: The generati<strong>on</strong> of global<br />

fields of terrestrial biophysical parameters from<br />

satellite data. Journal of Climate, Vol. 9, pp. 706-737,<br />

1996

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