KANZELHOHE_OBS







Location

lon / lat [deg]: 13.907 / 46.678

Source network: AERONET







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]:

1.73

Distance to urban areas [km]:

1.77



Radius: 1 km

Number of landcover classes:

3

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

85.0



Radius: 2 km

Number of landcover classes:

8

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

67.0



Radius: 5 km

Number of landcover classes:

8

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

50.0



Radius: 10 km

Number of landcover classes:

9

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

45.0



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 [%]:

45.0





Disturbances







Heterogeneity analysis

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

Topography



Roman et al. (2009) index


St

11.7632019451

Rcv

-0.0212539475361

Rse

0.0

Rst

-0.0167830840154

Rsv

-0.216995570456



Height range @ 1km [m]

1078

Height range @ 2km [m]

1252

Height range @ 5km [m]

1169

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

34470

Variance slope @ 2 km

41173

Variance slope @ 5 km

41502

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

21.482657022

Rcv

0.0297430214682

Rse

0.0

Rst

0.00482447291629

Rsv

-0.105080036036



NDVI range @ 1km [-]

0.05

NDVI range @ 2km [-]

0.08

NDVI range @ 5km [-]

0.1

NDVI range @ 10km [-]

0.12

NDVI range @ 20km [-]

0.12



Variance slope @ 1 km

0.000238521144494

Variance slope @ 2 km

0.000302763663454

Variance slope @ 5 km

0.000270044913548

Variance slope @ 10 km

0.000127873429366

Variance slope @ 20 km

5.27719392388e-05







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

8.23477531775

Rcv

0.107507535982

Rse

0.0

Rst

-0.0507212120991

Rsv

0.206079916605



NDVI range @ 1km [-]

0.15

NDVI range @ 2km [-]

0.18

NDVI range @ 5km [-]

0.24

NDVI range @ 10km [-]

0.21

NDVI range @ 20km [-]

0.23



NDVI slope @ 1 km

0.000750336251552

NDVI slope @ 2 km

0.000880027409466

NDVI slope @ 5 km

0.000695971774783

NDVI slope @ 10 km

0.000306930893588

NDVI slope @ 20 km

0.000158456645558







Temporal stability analysis

+000 deg (BHR)




BHR statistics

Temporal stability [1/decade]:


abs

rel


Weighted least square:

0.00246759924286






Ordinary least square:

-0.0131113674071










Probabilities that GCOS criteria is met:

Weighted least square:

0.0 %

Ordinary least square:

3.9 %





DHR statistics

Temporal stability [1/decade]:


abs

rel


Weighted least square:

-0.00170474957214






Ordinary least square:

-0.017099598874










Probabilities that GCOS criteria is met:

Weighted least square:

8.4 %

Ordinary least square:

3.7 %





+057/+063 deg (BHR)




BHR statistics

Temporal stability [1/decade]:


abs

rel


Weighted least square:

-0.00679006355426






Ordinary least square:

-0.0473293899183










Probabilities that GCOS criteria is met:

Weighted least square:

4.1 %

Ordinary least square:

4.4 %





DHR statistics

Temporal stability [1/decade]:


abs

rel


Weighted least square:

-0.00549981632212






Ordinary least square:

-0.0588031424833










Probabilities that GCOS criteria is met:

Weighted least square:

4.5 %

Ordinary least square:

4.5 %







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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