NAINITAL








Location

lon / lat [deg]: 79.4583 / 29.3588

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]:

2.58

Distance to urban areas [km]:

2.3



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 [%]:

53.0



Radius: 2 km

Number of landcover classes:

7

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

58.0



Radius: 5 km

Number of landcover classes:

11

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

48.0



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 [%]:

51.0



Radius: 20 km

Number of landcover classes:

11

Dominant landcover type:

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

Fraction of dominant landcover type [%]:

30.0





Disturbances









Heterogeneity analysis

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

Topography



Roman et al. (2009) index


St

1.96779959052

Rcv

0.494462573324

Rse

0.0

Rst

-0.030083360266

Rsv

-0.99999956101



Height range @ 1km [m]

349

Height range @ 2km [m]

631

Height range @ 5km [m]

1193

Height range @ 10km [m]

-999

Height range @ 20km [m]

-999



Variance slope @ 1 km

23199

Variance slope @ 2 km

23640

Variance slope @ 5 km

27942

Variance slope @ 10 km

-999

Variance slope @ 20 km

-999







NDVI (max. NDVI composite)


Roman et al. (2009) index


St

3.25896295219

Rcv

0.13421196942

Rse

0.0

Rst

0.0135877789866

Rsv

0.772738485384



NDVI range @ 1km [-]

0.04

NDVI range @ 2km [-]

0.11

NDVI range @ 5km [-]

0.17

NDVI range @ 10km [-]

0.13

NDVI range @ 20km [-]

0.16



Variance slope @ 1 km

0.000184793961585

Variance slope @ 2 km

0.000275104338952

Variance slope @ 5 km

0.000292637244235

Variance slope @ 10 km

0.000201075850443

Variance slope @ 20 km

0.00010282633831







NDVI (min. NDVI composite)I


Roman et al. (2009) index


St

8.26299977504

Rcv

0.172001064837

Rse

0.0

Rst

-0.0552947445303

Rsv

0.135768462892



NDVI range @ 1km [-]

0.04

NDVI range @ 2km [-]

0.06

NDVI range @ 5km [-]

0.12

NDVI range @ 10km [-]

0.12

NDVI range @ 20km [-]

0.22



NDVI slope @ 1 km

0.000379572967893

NDVI slope @ 2 km

0.000507949486074

NDVI slope @ 5 km

0.000543302250742

NDVI slope @ 10 km

0.000372780563169

NDVI slope @ 20 km

0.000167415831588







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:

-0.00786771338926






Ordinary least square:

-0.0406420783746










Probabilities that GCOS criteria is met:

Weighted least square:

2.8 %

Ordinary least square:

4.5 %





DHR statistics

Temporal stability [1/decade]:



abs

rel


Weighted least square:

-0.00363081067754






Ordinary least square:

-0.0394401422147










Probabilities that GCOS criteria is met:

Weighted least square:

4.5 %

Ordinary least square:

4.4 %







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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