BELMANIP_00405








Location

lon / lat [deg]: 63.848 / 63.4411

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]:

4.4

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 [%]:

94.0



Radius: 5 km

Number of landcover classes:

3

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

95.0



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 [%]:

97.0



Radius: 20 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





Disturbances









Heterogeneity analysis

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

Topography



Roman et al. (2009) index


St

0.968255061817

Rcv

0.150529060177

Rse

0.0

Rst

2.54773501792e-06

Rsv

2.94782554849



Height range @ 1km [m]

23

Height range @ 2km [m]

47

Height range @ 5km [m]

80

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

82

Variance slope @ 2 km

103

Variance slope @ 5 km

121

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

5.8275087339

Rcv

0.0371275276946

Rse

0.0

Rst

-0.121163792011

Rsv

0.356508423545



NDVI range @ 1km [-]

0.01

NDVI range @ 2km [-]

0.05

NDVI range @ 5km [-]

0.05

NDVI range @ 10km [-]

0.06

NDVI range @ 20km [-]

0.08



Variance slope @ 1 km

5.25073705841e-05

Variance slope @ 2 km

7.01132513361e-05

Variance slope @ 5 km

7.69182955412e-05

Variance slope @ 10 km

5.02970925585e-05

Variance slope @ 20 km

2.45547325894e-05







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

5.83146786122e-07

Rcv

-0.0711313190239

Rse

0.0

Rst

-0.0818507756383

Rsv

5144502.17712



NDVI range @ 1km [-]

0.02

NDVI range @ 2km [-]

0.08

NDVI range @ 5km [-]

0.1

NDVI range @ 10km [-]

0.11

NDVI range @ 20km [-]

0.15



NDVI slope @ 1 km

0.000274970506159

NDVI slope @ 2 km

0.000280091364652

NDVI slope @ 5 km

0.000199721643077

NDVI slope @ 10 km

0.0001125581232

NDVI slope @ 20 km

4.80128867142e-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