BELMANIP_00386








Location

lon / lat [deg]: 92.4166 / 59.3165

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]:

16.87

Distance to urban areas [km]:

none in region



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 [%]:

98.0



Radius: 5 km

Number of landcover classes:

1

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

99.0



Radius: 10 km

Number of landcover classes:

1

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

99.0



Radius: 20 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





Disturbances









Heterogeneity analysis

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

Topography



Roman et al. (2009) index


St

8.59204372771

Rcv

0.246239782543

Rse

0.0

Rst

0.0886947033392

Rsv

0.0142257482915



Height range @ 1km [m]

115

Height range @ 2km [m]

151

Height range @ 5km [m]

224

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

1747

Variance slope @ 2 km

1886

Variance slope @ 5 km

1164

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

3.1332867178

Rcv

-0.145028464871

Rse

0.0

Rst

0.260978823475

Rsv

-0.551453764597



NDVI range @ 1km [-]

0.02

NDVI range @ 2km [-]

0.04

NDVI range @ 5km [-]

0.05

NDVI range @ 10km [-]

0.05

NDVI range @ 20km [-]

0.07



Variance slope @ 1 km

5.30114601507e-05

Variance slope @ 2 km

5.27210439224e-05

Variance slope @ 5 km

4.20462638039e-05

Variance slope @ 10 km

2.24708077939e-05

Variance slope @ 20 km

1.3678224595e-05







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

2.01512218106

Rcv

-0.258664844231

Rse

0.0

Rst

0.671214091018

Rsv

-0.558864540552



NDVI range @ 1km [-]

0.05

NDVI range @ 2km [-]

0.06

NDVI range @ 5km [-]

0.1

NDVI range @ 10km [-]

0.08

NDVI range @ 20km [-]

0.1



NDVI slope @ 1 km

0.000331798816689

NDVI slope @ 2 km

0.000274741408277

NDVI slope @ 5 km

0.000129735248479

NDVI slope @ 10 km

4.41258296464e-05

NDVI slope @ 20 km

1.83100692543e-05







Temporal stability analysis

+000 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

None






Ordinary least square:

None










Probabilities that GCOS criteria is met:

Weighted least square:

None %

Ordinary least square:

None %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

None






Ordinary least square:

None










Probabilities that GCOS criteria is met:

Weighted least square:

None %

Ordinary least square:

None %





+057/+063 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

0.00432645062491






Ordinary least square:

-0.0332316798788










Probabilities that GCOS criteria is met:

Weighted least square:

4.6 %

Ordinary least square:

4.9 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

0.0137272437549






Ordinary least square:

-0.0232700032257










Probabilities that GCOS criteria is met:

Weighted least square:

0.1 %

Ordinary least square:

4.9 %







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