Hi all,
I’m working on an urban heat island mitigation study using the InVEST Urban Cooling Model, and I’d appreciate some feedback or suggestions.
What I’ve done so far:
-
I created a biophysical table based on FAO56 crop evapotranspiration data.
-
For each LULC class (agriculture, urban green, forest, etc.), I calculated a seasonal average Kc based on growth stages and durations.
-
I used a 5-month average Penman-Monteith reference ET₀ = 3.334 mm/day, computed from station data for the growing season (May to September).
-
I multiplied each land use’s Kc × 3.334 to get a proxy ET raster in mm/day.
Where I need help:
-
Is this a valid method to derive rasterized ET₀ input for the Urban Cooling model?
-
The model requires ET₀ as a raster layer (in mm/day), but my ET raster is Kc × average ET₀.
-
Would this be considered ETc instead? If yes, what’s the recommended way to get ET₀ as a raster?
-
-
How can I generate a spatially distributed raster of ET₀ (reference evapotranspiration)?
-
I’m using ArcGIS and QGIS.
-
Are there trusted global or regional raster datasets for ET₀?
-
Or should I interpolate ET₀ from nearby stations (I have daily values)?
-
-
Would it be better to use the Hargreaves method (less input data) instead of Penman-Monteith to create a monthly ET₀ raster?
NB
-
LULC map: 2m raster,
-
Reference ET data: May–Sept 2024 from station