BELMANIP_00273








Location

lon / lat [deg]: 58.3599 / 61.8885

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]:

10.56

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:

1

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

100.0



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 [%]:

100.0



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 [%]:

100.0



Radius: 20 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





Disturbances









Heterogeneity analysis

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

Topography



Roman et al. (2009) index


St

2.18498787989

Rcv

0.0111363084783

Rse

0.0

Rst

9.13234063565e-07

Rsv

1.36186810596



Height range @ 1km [m]

75

Height range @ 2km [m]

143

Height range @ 5km [m]

167

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

482

Variance slope @ 2 km

659

Variance slope @ 5 km

645

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

8.60240585866e-08

Rcv

0.00354572319891

Rse

0.0

Rst

0.0974946048568

Rsv

34873964.8024



NDVI range @ 1km [-]

0.02

NDVI range @ 2km [-]

0.04

NDVI range @ 5km [-]

0.05

NDVI range @ 10km [-]

0.06

NDVI range @ 20km [-]

0.06



Variance slope @ 1 km

4.45371039448e-05

Variance slope @ 2 km

4.96319611089e-05

Variance slope @ 5 km

3.84689988309e-05

Variance slope @ 10 km

2.13021885429e-05

Variance slope @ 20 km

1.03166894418e-05







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

17.8182766849

Rcv

-0.0196556716531

Rse

0.0

Rst

-0.0358059176959

Rsv

0.112904861182



NDVI range @ 1km [-]

0.02

NDVI range @ 2km [-]

0.05

NDVI range @ 5km [-]

0.07

NDVI range @ 10km [-]

0.08

NDVI range @ 20km [-]

0.11



NDVI slope @ 1 km

0.000116532286794

NDVI slope @ 2 km

0.00012693482092

NDVI slope @ 5 km

0.000110903962182

NDVI slope @ 10 km

8.2459578273e-05

NDVI slope @ 20 km

4.31424834906e-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