BELMANIP_00272








Location

lon / lat [deg]: 51.1818 / 64.1696

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]:

30.61

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:

2

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

3.76478797493

Rcv

0.158599766715

Rse

0.0

Rst

-0.0773805249782

Rsv

0.560877332156



Height range @ 1km [m]

22

Height range @ 2km [m]

35

Height range @ 5km [m]

47

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

81

Variance slope @ 2 km

72

Variance slope @ 5 km

49

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

3.68959088111e-07

Rcv

0.61421571068

Rse

0.0

Rst

0.122000509208

Rsv

8130982.0656



NDVI range @ 1km [-]

0.02

NDVI range @ 2km [-]

0.02

NDVI range @ 5km [-]

0.06

NDVI range @ 10km [-]

0.06

NDVI range @ 20km [-]

0.06



Variance slope @ 1 km

6.24281809921e-05

Variance slope @ 2 km

6.54689781527e-05

Variance slope @ 5 km

4.94301014327e-05

Variance slope @ 10 km

2.37236878829e-05

Variance slope @ 20 km

1.04102555557e-05







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

2.8697292357

Rcv

-0.0452653650577

Rse

0.0

Rst

-0.000130100281585

Rsv

-0.999999327549



NDVI range @ 1km [-]

0.08

NDVI range @ 2km [-]

0.14

NDVI range @ 5km [-]

0.13

NDVI range @ 10km [-]

0.12

NDVI range @ 20km [-]

0.2



NDVI slope @ 1 km

0.000579871022705

NDVI slope @ 2 km

0.000526317699901

NDVI slope @ 5 km

0.00028279119885

NDVI slope @ 10 km

0.000118900732661

NDVI slope @ 20 km

4.96322045615e-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