BELMANIP_00259








Location

lon / lat [deg]: 9.7255 / 59.4004

Source network: BELMANIP







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]:

1.64

Distance to urban areas [km]:

9.54



Radius: 1 km

Number of landcover classes:

1

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

100.0



Radius: 2 km

Number of landcover classes:

2

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

97.0



Radius: 5 km

Number of landcover classes:

2

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

93.0



Radius: 10 km

Number of landcover classes:

3

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

92.0



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 [%]:

84.0





Disturbances









Heterogeneity analysis

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

Topography



Roman et al. (2009) index


St

11.9611241358

Rcv

0.0916847442688

Rse

0.0

Rst

-0.0425915954139

Rsv

0.116536206524



Height range @ 1km [m]

119

Height range @ 2km [m]

172

Height range @ 5km [m]

215

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

2179

Variance slope @ 2 km

2034

Variance slope @ 5 km

916

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

3.48972070437e-07

Rcv

1.2189516711

Rse

0.0

Rst

-0.0370924509352

Rsv

8596675.25232



NDVI range @ 1km [-]

0.03

NDVI range @ 2km [-]

0.03

NDVI range @ 5km [-]

0.05

NDVI range @ 10km [-]

0.08

NDVI range @ 20km [-]

0.12



Variance slope @ 1 km

9.88674454176e-05

Variance slope @ 2 km

0.000109538579758

Variance slope @ 5 km

0.000111106851011

Variance slope @ 10 km

8.74611313871e-05

Variance slope @ 20 km

7.51934493517e-05







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

1.70599315329

Rcv

-0.0174708549835

Rse

0.0

Rst

-0.331271322886

Rsv

1.4097642934



NDVI range @ 1km [-]

0.16

NDVI range @ 2km [-]

0.18

NDVI range @ 5km [-]

0.17

NDVI range @ 10km [-]

0.21

NDVI range @ 20km [-]

0.23



NDVI slope @ 1 km

0.000686351368244

NDVI slope @ 2 km

0.00070354148564

NDVI slope @ 5 km

0.000558799320622

NDVI slope @ 10 km

0.000256893086815

NDVI slope @ 20 km

0.000187531921293







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