SE-FLA








Location

lon / lat [deg]: 19.4569 / 64.1128

Source network: FLUXNET







Geostationary surface albedo (GSA) data


“+000”


“+057/+063”


Landcover information (based on ESA CCI landcover data)


Landcover fractions @ 2km distance


Landcover fractions @ 20 km distance




Legend



Distance to open water bodies [km]:

1.83

Distance to urban areas [km]:

10.25



Radius: 1 km

Number of landcover classes:

3

Dominant landcover type:

70: Tree cover, needleleaved, evergreen, closed to open (>15%)

Fraction of dominant landcover type [%]:

91.0



Radius: 2 km

Number of landcover classes:

5

Dominant landcover type:

70: Tree cover, needleleaved, evergreen, closed to open (>15%)

Fraction of dominant landcover type [%]:

89.0



Radius: 5 km

Number of landcover classes:

4

Dominant landcover type:

70: Tree cover, needleleaved, evergreen, closed to open (>15%)

Fraction of dominant landcover type [%]:

90.0



Radius: 10 km

Number of landcover classes:

5

Dominant landcover type:

70: Tree cover, needleleaved, evergreen, closed to open (>15%)

Fraction of dominant landcover type [%]:

88.0



Radius: 20 km

Number of landcover classes:

5

Dominant landcover type:

70: Tree cover, needleleaved, evergreen, closed to open (>15%)

Fraction of dominant landcover type [%]:

89.0





Disturbances









Heterogeneity analysis

The heterogeneity analysis provides information about the spatial and temporal heterogeneity of the site.

Topography



Roman et al. (2009) index


St

6.66086924044

Rcv

0.0404772679299

Rse

0.0

Rst

-0.0341145357625

Rsv

0.375799863177



Height range @ 1km [m]

58

Height range @ 2km [m]

93

Height range @ 5km [m]

102

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

528

Variance slope @ 2 km

527

Variance slope @ 5 km

209

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

20.1264255441

Rcv

-0.0399215302817

Rse

0.0

Rst

-0.0246688940228

Rsv

0.0844673402459



NDVI range @ 1km [-]

0.04

NDVI range @ 2km [-]

0.07

NDVI range @ 5km [-]

0.08

NDVI range @ 10km [-]

0.06

NDVI range @ 20km [-]

0.07



Variance slope @ 1 km

9.55213866455e-05

Variance slope @ 2 km

0.000103760054573

Variance slope @ 5 km

6.76894687601e-05

Variance slope @ 10 km

2.70297765382e-05

Variance slope @ 20 km

1.12418455254e-05







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

6.29213178982

Rcv

0.00953657612216

Rse

0.0

Rst

0.205132912423

Rsv

-0.262116456221



NDVI range @ 1km [-]

0.08

NDVI range @ 2km [-]

0.12

NDVI range @ 5km [-]

0.15

NDVI range @ 10km [-]

0.18

NDVI range @ 20km [-]

0.18



NDVI slope @ 1 km

0.000943413685367

NDVI slope @ 2 km

0.000864768332032

NDVI slope @ 5 km

0.000478111227746

NDVI slope @ 10 km

0.000247121877031

NDVI slope @ 20 km

9.69488366978e-05







Temporal stability analysis

+000 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-99999.0






Ordinary least square:

-99999.0










Probabilities that GCOS criteria is met:

Weighted least square:

-99999.0 %

Ordinary least square:

-99999.0 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-99999.0






Ordinary least square:

-99999.0










Probabilities that GCOS criteria is met:

Weighted least square:

-99999.0 %

Ordinary least square:

-99999.0 %





+057/+063 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-99999.0






Ordinary least square:

-99999.0










Probabilities that GCOS criteria is met:

Weighted least square:

-99999.0 %

Ordinary least square:

-99999.0 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-99999.0






Ordinary least square:

-99999.0










Probabilities that GCOS criteria is met:

Weighted least square:

-99999.0 %

Ordinary least square:

-99999.0 %







Temporal anomaly analyis

The variance of the temporal anomalies provides an additional measure about the stability of the signal AFTER removal of the mean seasonal cylce.

+000 deg


+057/+063 deg