| Associated entities to this dataset: |
| Attribute Name -- Attribute Label |
Unit |
Attribute definition |
Huma
--
Air humidity
|
Percent |
Relative humidity of the air |
|
Method
(Sampling/processing description of the values of
this attribute by one ore more steps.)
|
|
--- Step
1
---
|
|
Title
:
|
calculating spatial relaive humidity and specific saturation deficit maps |
|
Description
:
|
Regionalization of humiditiy and saturation deficit as average monthly mean, minimum, and maximum maps by combining a straightforward detrending technique with a Digital Elevation Model and a sattelite-based land cover classification.
- calculation of monthly RH averages
- interpolation (Kriging) of the detrended data resulting in four maps for th different land cover units
- altitudinal distribution of humidity is reconstructed by using the DEM
- deriving RH maps for inside and outside the forest considering the vegetation distribution
- to detrmine saturation vapor pressure (E), temperatur maps are used ("Fries A. (2011): Air temperature maps (monthly and annual averages of mean, min, max) based on observation data (1999-2009) and topography . Available online (http://www.tropicalmountainforest.org/data_pre.do?citid=1054) from DFG-FOR816dw.)"
- the E-Maps in combination with the near surface RH-Maps are also used to detrmine the actual water vapor pressure (e)
- e-Maps are the basis for the calculation of the saturation specific humidity (Q)
- the specific saturation deficit (Ds) is determined by using Q- and q-Maps
The single steps are described in more detail in the cited article. |
|
Citation:
|
Fries, A
.
,
Rollenbeck, R
.
,
Nauss, T
.
,
Peters, T
.
,
and
Bendix, J
.
(2012):
Near surface air humidity in a megadiverse Andean mountain ecosystem of southern Ecuador and its regionalization.
. Available online
(http://tropicalmountainforest.org/publications.do?citid=1020) from DFG-FOR816dw.
|
|
|
|
|
|
| Attribute Name -- Attribute Label |
Unit |
Attribute definition |
Huma
--
Air humidity
|
Percent |
Relative humidity of the air |
|
Method
(Sampling/processing description of the values of
this attribute by one ore more steps.)
|
|
--- Step
1
---
|
|
Title
:
|
calculating spatial relaive humidity and specific saturation deficit maps |
|
Description
:
|
Regionalization of humiditiy and saturation deficit as average monthly mean, minimum, and maximum maps by combining a straightforward detrending technique with a Digital Elevation Model and a sattelite-based land cover classification.
- calculation of monthly RH averages
- interpolation (Kriging) of the detrended data resulting in four maps for th different land cover units
- altitudinal distribution of humidity is reconstructed by using the DEM
- deriving RH maps for inside and outside the forest considering the vegetation distribution
- to detrmine saturation vapor pressure (E), temperatur maps are used ("Fries A. (2011): Air temperature maps (monthly and annual averages of mean, min, max) based on observation data (1999-2009) and topography . Available online (http://www.tropicalmountainforest.org/data_pre.do?citid=1054) from DFG-FOR816dw.)"
- the E-Maps in combination with the near surface RH-Maps are also used to detrmine the actual water vapor pressure (e)
- e-Maps are the basis for the calculation of the saturation specific humidity (Q)
- the specific saturation deficit (Ds) is determined by using Q- and q-Maps
The single steps are described in more detail in the cited article. |
|
Citation:
|
Fries, A
.
,
Rollenbeck, R
.
,
Nauss, T
.
,
Peters, T
.
,
and
Bendix, J
.
(2012):
Near surface air humidity in a megadiverse Andean mountain ecosystem of southern Ecuador and its regionalization.
. Available online
(http://tropicalmountainforest.org/publications.do?citid=1020) from DFG-FOR816dw.
|
|
|
|
|
|
| Attribute Name -- Attribute Label |
Unit |
Attribute definition |
Huma
--
Air humidity
|
Percent |
Relative humidity of the air |
|
Method
(Sampling/processing description of the values of
this attribute by one ore more steps.)
|
|
--- Step
1
---
|
|
Title
:
|
calculating spatial relaive humidity and specific saturation deficit maps |
|
Description
:
|
Regionalization of humiditiy and saturation deficit as average monthly mean, minimum, and maximum maps by combining a straightforward detrending technique with a Digital Elevation Model and a sattelite-based land cover classification.
- calculation of monthly RH averages
- interpolation (Kriging) of the detrended data resulting in four maps for th different land cover units
- altitudinal distribution of humidity is reconstructed by using the DEM
- deriving RH maps for inside and outside the forest considering the vegetation distribution
- to detrmine saturation vapor pressure (E), temperatur maps are used ("Fries A. (2011): Air temperature maps (monthly and annual averages of mean, min, max) based on observation data (1999-2009) and topography . Available online (http://www.tropicalmountainforest.org/data_pre.do?citid=1054) from DFG-FOR816dw.)"
- the E-Maps in combination with the near surface RH-Maps are also used to detrmine the actual water vapor pressure (e)
- e-Maps are the basis for the calculation of the saturation specific humidity (Q)
- the specific saturation deficit (Ds) is determined by using Q- and q-Maps
The single steps are described in more detail in the cited article. |
|
Citation:
|
Fries, A
.
,
Rollenbeck, R
.
,
Nauss, T
.
,
Peters, T
.
,
and
Bendix, J
.
(2012):
Near surface air humidity in a megadiverse Andean mountain ecosystem of southern Ecuador and its regionalization.
. Available online
(http://tropicalmountainforest.org/publications.do?citid=1020) from DFG-FOR816dw.
|
|
|
|
|
|
| Attribute Name -- Attribute Label |
Unit |
Attribute definition |
Huma
--
Air humidity
|
Percent |
Relative humidity of the air |
|
Method
(Sampling/processing description of the values of
this attribute by one ore more steps.)
|
|
--- Step
1
---
|
|
Title
:
|
calculating spatial relaive humidity and specific saturation deficit maps |
|
Description
:
|
Regionalization of humiditiy and saturation deficit as average monthly mean, minimum, and maximum maps by combining a straightforward detrending technique with a Digital Elevation Model and a sattelite-based land cover classification.
- calculation of monthly RH averages
- interpolation (Kriging) of the detrended data resulting in four maps for th different land cover units
- altitudinal distribution of humidity is reconstructed by using the DEM
- deriving RH maps for inside and outside the forest considering the vegetation distribution
- to detrmine saturation vapor pressure (E), temperatur maps are used ("Fries A. (2011): Air temperature maps (monthly and annual averages of mean, min, max) based on observation data (1999-2009) and topography . Available online (http://www.tropicalmountainforest.org/data_pre.do?citid=1054) from DFG-FOR816dw.)"
- the E-Maps in combination with the near surface RH-Maps are also used to detrmine the actual water vapor pressure (e)
- e-Maps are the basis for the calculation of the saturation specific humidity (Q)
- the specific saturation deficit (Ds) is determined by using Q- and q-Maps
The single steps are described in more detail in the cited article. |
|
Citation:
|
Fries, A
.
,
Rollenbeck, R
.
,
Nauss, T
.
,
Peters, T
.
,
and
Bendix, J
.
(2012):
Near surface air humidity in a megadiverse Andean mountain ecosystem of southern Ecuador and its regionalization.
. Available online
(http://tropicalmountainforest.org/publications.do?citid=1020) from DFG-FOR816dw.
|
|
|
|
|
|
| Attribute Name -- Attribute Label |
Unit |
Attribute definition |
Huma
--
Air humidity
|
Percent |
Relative humidity of the air |
|
Method
(Sampling/processing description of the values of
this attribute by one ore more steps.)
|
|
--- Step
1
---
|
|
Title
:
|
calculating spatial relaive humidity and specific saturation deficit maps |
|
Description
:
|
Regionalization of humiditiy and saturation deficit as average monthly mean, minimum, and maximum maps by combining a straightforward detrending technique with a Digital Elevation Model and a sattelite-based land cover classification.
- calculation of monthly RH averages
- interpolation (Kriging) of the detrended data resulting in four maps for th different land cover units
- altitudinal distribution of humidity is reconstructed by using the DEM
- deriving RH maps for inside and outside the forest considering the vegetation distribution
- to detrmine saturation vapor pressure (E), temperatur maps are used ("Fries A. (2011): Air temperature maps (monthly and annual averages of mean, min, max) based on observation data (1999-2009) and topography . Available online (http://www.tropicalmountainforest.org/data_pre.do?citid=1054) from DFG-FOR816dw.)"
- the E-Maps in combination with the near surface RH-Maps are also used to detrmine the actual water vapor pressure (e)
- e-Maps are the basis for the calculation of the saturation specific humidity (Q)
- the specific saturation deficit (Ds) is determined by using Q- and q-Maps
The single steps are described in more detail in the cited article. |
|
Citation:
|
Fries, A
.
,
Rollenbeck, R
.
,
Nauss, T
.
,
Peters, T
.
,
and
Bendix, J
.
(2012):
Near surface air humidity in a megadiverse Andean mountain ecosystem of southern Ecuador and its regionalization.
. Available online
(http://tropicalmountainforest.org/publications.do?citid=1020) from DFG-FOR816dw.
|
|
|
|
|
|
| Attribute Name -- Attribute Label |
Unit |
Attribute definition |
Huma
--
Air humidity
|
Percent |
Relative humidity of the air |
|
Method
(Sampling/processing description of the values of
this attribute by one ore more steps.)
|
|
--- Step
1
---
|
|
Title
:
|
calculating spatial relaive humidity and specific saturation deficit maps |
|
Description
:
|
Regionalization of humiditiy and saturation deficit as average monthly mean, minimum, and maximum maps by combining a straightforward detrending technique with a Digital Elevation Model and a sattelite-based land cover classification.
- calculation of monthly RH averages
- interpolation (Kriging) of the detrended data resulting in four maps for th different land cover units
- altitudinal distribution of humidity is reconstructed by using the DEM
- deriving RH maps for inside and outside the forest considering the vegetation distribution
- to detrmine saturation vapor pressure (E), temperatur maps are used ("Fries A. (2011): Air temperature maps (monthly and annual averages of mean, min, max) based on observation data (1999-2009) and topography . Available online (http://www.tropicalmountainforest.org/data_pre.do?citid=1054) from DFG-FOR816dw.)"
- the E-Maps in combination with the near surface RH-Maps are also used to detrmine the actual water vapor pressure (e)
- e-Maps are the basis for the calculation of the saturation specific humidity (Q)
- the specific saturation deficit (Ds) is determined by using Q- and q-Maps
The single steps are described in more detail in the cited article. |
|
Citation:
|
Fries, A
.
,
Rollenbeck, R
.
,
Nauss, T
.
,
Peters, T
.
,
and
Bendix, J
.
(2012):
Near surface air humidity in a megadiverse Andean mountain ecosystem of southern Ecuador and its regionalization.
. Available online
(http://tropicalmountainforest.org/publications.do?citid=1020) from DFG-FOR816dw.
|
|
|
|
|
|
| Attribute Name -- Attribute Label |
Unit |
Attribute definition |
d
--
Deficit of specific humidity
|
Gram per kilogram |
Deficit of specific humidity |
|
Method
(Sampling/processing description of the values of
this attribute by one ore more steps.)
|
|
--- Step
1
---
|
|
Title
:
|
calculating spatial relaive humidity and specific saturation deficit maps |
|
Description
:
|
Regionalization of humiditiy and saturation deficit as average monthly mean, minimum, and maximum maps by combining a straightforward detrending technique with a Digital Elevation Model and a sattelite-based land cover classification.
- calculation of monthly RH averages
- interpolation (Kriging) of the detrended data resulting in four maps for th different land cover units
- altitudinal distribution of humidity is reconstructed by using the DEM
- deriving RH maps for inside and outside the forest considering the vegetation distribution
- to detrmine saturation vapor pressure (E), temperatur maps are used ("Fries A. (2011): Air temperature maps (monthly and annual averages of mean, min, max) based on observation data (1999-2009) and topography . Available online (http://www.tropicalmountainforest.org/data_pre.do?citid=1054) from DFG-FOR816dw.)"
- the E-Maps in combination with the near surface RH-Maps are also used to detrmine the actual water vapor pressure (e)
- e-Maps are the basis for the calculation of the saturation specific humidity (Q)
- the specific saturation deficit (Ds) is determined by using Q- and q-Maps
The single steps are described in more detail in the cited article. |
|
Citation:
|
Fries, A
.
,
Rollenbeck, R
.
,
Nauss, T
.
,
Peters, T
.
,
and
Bendix, J
.
(2012):
Near surface air humidity in a megadiverse Andean mountain ecosystem of southern Ecuador and its regionalization.
. Available online
(http://tropicalmountainforest.org/publications.do?citid=1020) from DFG-FOR816dw.
|
|
|
|
|
|
| Attribute Name -- Attribute Label |
Unit |
Attribute definition |
|
|
|
|
