BELMANIP_00372







Location

lon / lat [deg]: 107.26 / 40.9604

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]:

3.45

Distance to urban areas [km]:

9.05



Radius: 1 km

Number of landcover classes:

3

Dominant landcover type:

40: mosaic natural vegetation (tree, shrub, herbaceous cover) (>50%) / cropland (<50%)

Fraction of dominant landcover type [%]:

68.0



Radius: 2 km

Number of landcover classes:

4

Dominant landcover type:

40: mosaic natural vegetation (tree, shrub, herbaceous cover) (>50%) / cropland (<50%)

Fraction of dominant landcover type [%]:

74.0



Radius: 5 km

Number of landcover classes:

6

Dominant landcover type:

40: mosaic natural vegetation (tree, shrub, herbaceous cover) (>50%) / cropland (<50%)

Fraction of dominant landcover type [%]:

65.0



Radius: 10 km

Number of landcover classes:

5

Dominant landcover type:

40: mosaic natural vegetation (tree, shrub, herbaceous cover) (>50%) / cropland (<50%)

Fraction of dominant landcover type [%]:

62.0



Radius: 20 km

Number of landcover classes:

6

Dominant landcover type:

40: mosaic natural vegetation (tree, shrub, herbaceous cover) (>50%) / cropland (<50%)

Fraction of dominant landcover type [%]:

48.0





Disturbances







Heterogeneity analysis

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

Topography



Roman et al. (2009) index


St

2.00709093318

Rcv

0.0900976637441

Rse

0.0

Rst

-0.404610252321

Rsv

-0.999992672936



Height range @ 1km [m]

3

Height range @ 2km [m]

4

Height range @ 5km [m]

4

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

0

Variance slope @ 2 km

0

Variance slope @ 5 km

0

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

2.04766682703

Rcv

0.296108686842

Rse

0.0

Rst

-0.168973522249

Rsv

-0.99999988356



NDVI range @ 1km [-]

0.01

NDVI range @ 2km [-]

0.04

NDVI range @ 5km [-]

0.08

NDVI range @ 10km [-]

0.12

NDVI range @ 20km [-]

0.14



Variance slope @ 1 km

0.000399863036924

Variance slope @ 2 km

0.000414247696205

Variance slope @ 5 km

0.000354232703276

Variance slope @ 10 km

0.000170330784267

Variance slope @ 20 km

5.77872937096e-05







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

0.43869168587

Rcv

0.816790952029

Rse

0.0

Rst

-0.647729653001

Rsv

5.37399513763



NDVI range @ 1km [-]

0.0

NDVI range @ 2km [-]

0.01

NDVI range @ 5km [-]

0.02

NDVI range @ 10km [-]

0.02

NDVI range @ 20km [-]

0.02



NDVI slope @ 1 km

9.59663649492e-06

NDVI slope @ 2 km

9.05642475013e-06

NDVI slope @ 5 km

6.3525646506e-06

NDVI slope @ 10 km

3.44991346069e-06

NDVI slope @ 20 km

1.68353683917e-06







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:

-0.0345795607302






Ordinary least square:

-0.00522239422439










Probabilities that GCOS criteria is met:

Weighted least square:

3.6 %

Ordinary least square:

4.8 %





DHR statistics

Temporal stability [1/decade]:


abs

rel


Weighted least square:

-0.0308173601262






Ordinary least square:

-0.00359760077128










Probabilities that GCOS criteria is met:

Weighted least square:

3.7 %

Ordinary least square:

5.0 %







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






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