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Compare PET
TerraClimate provide PET at 4 x 4 km based on Penman Montieth
We can compute PET with Thornwaite based only on T and Lat
or with hargraeaves with tmin tmax and radiation (from WC mean over the period at 1x1km (kJ m-2 day-1) or time varying srad at 2 x 2 km from TerraClimate srad Downward surface shortwave radiation), units = W/m2).
We can compte these PET with this package https://rdrr.io/cran/SPEI/man/PET.html
Sum of growing degree days from monthly mean
In CHELSA
We interpolated mean monthly temperatures
(t) to a daily resolution using a B-cubic spline interpolation and used this as input data for the
growing degree days.
See also review of method by Julien
ERA5 land
Should we explore ERA5 - land as well (11 x 11 km but dowscaling possible )
Unit Terraclimate
aet (Actual Evapotranspiration, monthly total), units = mm
def (Climate Water Deficit, monthly total), units = mm
pet (Potential evapotranspiration, monthly total), units = mm
ppt (Precipitation, monthly total), units = mm
q (Runoff, monthly total), units = mm
soil (Soil Moisture, total column - at end of month), units = mm
srad (Downward surface shortwave radiation), units = W/m2
swe (Snow water equivalent - at end of month), units = mm
tmax (Max Temperature, average for month), units = C
tmin (Min Temperature, average for month), units = C
vap (Vapor pressure, average for month), units = kPa
ws (Wind speed, average for month), units = m/s
vpd (Vapor Pressure Deficit, average for month), units = kpa
PDSI (Palmer Drought Severity Index, at end of month), units = unitless
Compute minimum soil water potential Soil PSI min
Benito Garzon et al. 2017 GEB computed Soil PSI min from
-
ERA-INTERIM volumetric soil water content (spatial resolution (10 x 15 km)
https://apps.ecmwf.int/datasets/data/interim-full-daily/levtype=sfc/ -
Soil water texture data from JRC Europe
http://eusoils.jrc.ec.europa.eu/wrb/
https://esdac.jrc.ec.europa.eu/content/european-soil-database-v2-raster-library-1kmx1km
https://esdac.jrc.ec.europa.eu/content/sgdbe-attributes#TEXT_SRF_DOM dominant surface
The for each plot the max volumetric soil water content Wmax was computed as mean of monthly data for 5 wetter year and minimum for 5 driest year Wmin. For each soil category computed water potential at maximum hydratation PSImax
Then PSImin is computed PSImin = PSImax * (Wmin/Wmax)^b with b computed per soil type.
Extrac soil data
UPDATE download command
wget -P data/ --no-host-directories --force-directories --input-file=envidatS3paths_all.txt
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