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David Schäfer authored6a6134bc
Soil Moisture
A collection of soil moisture specific quality check routines.
Index
- soilMoisture_spikes
- soilMoisture_breaks
- soilMoisture_constant
- soilMoisture_byFrost
- soilMoisture_byPrecipitation
soilMoisture_spikes
soilMoisture_spikes(raise_factor=0.15, deriv_factor=0.2,
noise_func="CoVar", noise_window="12h", noise_thresh=1,
smooth_window="3h")
parameter | default value |
---|---|
raise_factor | 0.15 |
deriv_factor | 0.2 |
noise_thresh | 1 |
noise_window | "12h" |
noise_func | "CoVar" |
smooth_window | "3h" |
The Function is a wrapper around flagSpikes_spektrumBased
with a set of default parameters referring to [1]. For a complete description of
the algorithm and the available parameters please refer to the documentation of
flagSpikes_spektrumBased
[1] Dorigo, W. et al: Global Automated Quality Control of In Situ Soil Moisture Data from the international Soil Moisture Network. 2013. Vadoze Zone J. doi:10.2136/vzj2012.0097.
soilMoisture_breaks
soilMoisture_breaks(thresh_rel=0.1, thresh_abs=0.01,
first_der_factor=10, first_der_window="12h",
scnd_der_ratio_range=0.05, scnd_der_ratio_thresh=10,
smooth=False, smooth_window="3h", smooth_poly_deg=2)
parameter | default value |
---|---|
thresh_rel | 0.1 |
thresh_abs | 0.01 |
first_der_factor | 10 |
first_der_window | "12h" |
scnd_der_ratio_range | 0.05 |
scnd_der_ratio_thresh | 10.0 |
smooth | False |
smooth_window | "3h" |
smooth_poly_deg | 2 |
The Function is a wrapper around breaks_spektrumBased
with a set of default parameters referring to [1]. For a complete description of
the algorithm and the available parameters please refer to the documentation of
breaks_spektrumBased.
[1] Dorigo, W. et al: Global Automated Quality Control of In Situ Soil Moisture Data from the international Soil Moisture Network. 2013. Vadoze Zone J. doi:10.2136/vzj2012.0097.
soilMoisture_constant
soilMoisture_constant(window="12h", thresh=0.0005,
precipitation_window="12h",
tolerance=0.95,
deriv_max=0.0025, deriv_min=0,
max_missing=None, max_consec_missing=None,
smooth_window=None, smooth_poly_deg=2)
parameter | data type | default value | description |
---|---|---|---|
window | offset string | Minimum duration during which values need to identical to become plateau candidates. See condition (1) | |
thresh | float | 0.0005 |
Maximum variance of a group of values to still consider them constant. See condition (2) |
precipitation_window | offset string | "12h" |
See condition (3) and (4) |
tolerance | float | 0.95 |
Tolerance factor, see condition (5) |
deriv_min | float | 0.0025 |
See condition (3) |
deriv_max | float | 0 |
See condition (4) |
max_missing | integer | None |
Maximum number of missing values allowed in window , by default this condition is ignored |
max_consec_missing | integer | None |
Maximum number of consecutive missing values allowed in window , by default this condition is ignored |
smooth_window | offset string | None |
Size of the smoothing window of the Savitsky-Golay filter. The default value None results in a window of two times the sampling rate (i.e. three values) |
smooth_poly_deg | integer | 2 |
Degree of the polynomial used for smoothing with the Savitsky-Golay filter |
This function flags plateaus/series of constant values in soil moisture data.
The function represents a stricter version of constant_varianceBased. The additional constraints (3)-(5), are designed to match the special cases of constant values in soil moisture measurements and basically for preceding precipitation events (conditions (3) and (4)) and certain plateau level (condition (5)).
Any set of consecutive values
-
window
-
thresh
-
deriv_min
, withdenoting periods perprecipitation_window
-
deriv_max
, withdenoting periods perprecipitation_window
-
tolerance
NOTE:
- The time series is expected to be harmonized to an equidistant frequency grid
This Function is based on [1] and all default parameter values are taken from this publication.
[1] Dorigo, W. et al: Global Automated Quality Control of In Situ Soil Moisture Data from the international Soil Moisture Network. 2013. Vadoze Zone J. doi:10.2136/vzj2012.0097.
soilMoisture_byFrost
soilMoisture_byFrost(soil_temp_variable, window="1h", frost_thresh=0)
parameter | data type | default value | description |
---|---|---|---|
soil_temp_variable | string | Name of the soil temperature variable in the dataset | |
window | offset string | "1h" |
Window around a value checked for frost events |
frost_thresh | float | 0 |
Soil temperature below frost_thresh are considered as frost |
This function flags soil moisture values if the soil temperature
(given in soil_temp_variable
) drops below frost_thresh
within a period of +/- window
.
This Function is an implementation of the soil temperature based flagging presented in [1] and all default parameter values are taken from this publication.
[1] Dorigo, W. et al: Global Automated Quality Control of In Situ Soil Moisture Data from the international Soil Moisture Network. 2013. Vadoze Zone J. doi:10.2136/vzj2012.0097.
soilMoisture_byPrecipitation
soilMoisture_byPrecipitation(prec_variable, sensor_depth=0,
raise_window=None,
sensor_accuracy=0, soil_porosity=0,
std_factor=2, std_window="24h"
ignore_missing=False)
parameter | data type | default value | description |
---|---|---|---|
prec_variable | string | Name of the precipitation variable in the dataset | |
raise_window | offset string | None |
Duration during which a rise has to occur |
sensor_depth | float | 0 |
Depth of the soil moisture sensor in meter |
sensor_accuracy | float | 0 |
Soil moisture sensor accuracy in |
soil_porosity | float | 0 |
Porosity of the soil surrounding the soil moisture sensor |
std_factor | integer | 2 |
See condition (2) |
std_window | offset string | "1h" |
See condition (2) |
ignore_missing | bool | False |
Whether to check values even if there is invalid data within std_window
|
This function flags rises in soil moisture data if there are no sufficiently large precipitation events in the preceding 24 hours.
A data point
-
x_krepresents a rise in soil moisture, i.e. fors =(
raise_window
/f):x_k > x_{k-s} -
The rise is sufficiently large and exceeds a threshold based on the standard deviation
\sigmaof the values in the precedingstd_window
, i.e. the following condition is fulfilled forh =std_window
/f:x_k - x_{k-s} >std_factor
\cdot \sigma(x_{t-h},...,x_{k}) -
The total amount of precipitation within the last 24 hours does not exceed a certain threshold, i.e. with
j ="24h" /fthe following condition is fulfilled:y_{k-j} + y_{k-j+1} + ... + y_{k} \lesensor_depth
\cdotsensor_accuracy
\cdotsoil_porosity
This Function is an implementation of the precipitation based flagging presented in [1] and all default parameter values are taken from this publication.
[1] Dorigo, W. et al: Global Automated Quality Control of In Situ Soil Moisture Data from the international Soil Moisture Network. 2013. Vadoze Zone J. doi:10.2136/vzj2012.0097.