CZ-BK1








Location

lon / lat [deg]: 18.5384 / 49.5026

Source network: FLUXNET







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]:

7.35

Distance to urban areas [km]:

0.56



Radius: 1 km

Number of landcover classes:

2

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

92.0



Radius: 2 km

Number of landcover classes:

3

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

96.0



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 [%]:

97.0



Radius: 10 km

Number of landcover classes:

5

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

82.0



Radius: 20 km

Number of landcover classes:

9

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

57.0





Disturbances









Heterogeneity analysis

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

Topography



Roman et al. (2009) index


St

2.06016538009

Rcv

0.281554934073

Rse

0.0

Rst

-0.150982374354

Rsv

1.02365646562



Height range @ 1km [m]

181

Height range @ 2km [m]

208

Height range @ 5km [m]

312

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

4487

Variance slope @ 2 km

3698

Variance slope @ 5 km

1868

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

0.931614251449

Rcv

0.537822374471

Rse

0.0

Rst

-0.566724095775

Rsv

2.11567047613



NDVI range @ 1km [-]

0.02

NDVI range @ 2km [-]

0.02

NDVI range @ 5km [-]

0.03

NDVI range @ 10km [-]

0.06

NDVI range @ 20km [-]

0.07



Variance slope @ 1 km

5.74657725252e-05

Variance slope @ 2 km

6.28455030023e-05

Variance slope @ 5 km

5.46487061149e-05

Variance slope @ 10 km

3.67471391241e-05

Variance slope @ 20 km

2.53346646465e-05







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

0.659408589117

Rcv

0.272808062041

Rse

0.0

Rst

-0.751772490504

Rsv

3.52495072368



NDVI range @ 1km [-]

0.06

NDVI range @ 2km [-]

0.08

NDVI range @ 5km [-]

0.12

NDVI range @ 10km [-]

0.12

NDVI range @ 20km [-]

0.12



NDVI slope @ 1 km

0.00024543945497

NDVI slope @ 2 km

0.000264848811286

NDVI slope @ 5 km

0.000177368259709

NDVI slope @ 10 km

8.6428306764e-05

NDVI slope @ 20 km

4.5186755682e-05







Temporal stability analysis

+000 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.00807058610899






Ordinary least square:

0.0103179090902










Probabilities that GCOS criteria is met:

Weighted least square:

2.9 %

Ordinary least square:

0.5 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.0095407409764






Ordinary least square:

0.00630347761312










Probabilities that GCOS criteria is met:

Weighted least square:

2.9 %

Ordinary least square:

3.1 %





+057/+063 deg (BHR)




BHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.0285440342912






Ordinary least square:

-0.0472794825098










Probabilities that GCOS criteria is met:

Weighted least square:

3.9 %

Ordinary least square:

4.5 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.0247927442805






Ordinary least square:

-0.0419656646399










Probabilities that GCOS criteria is met:

Weighted least square:

3.9 %

Ordinary least square:

4.6 %







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