You signed in with another tab or window. Reload to refresh your session.You signed out in another tab or window. Reload to refresh your session.You switched accounts on another tab or window. Reload to refresh your session.Dismiss alert
Copy file name to clipboardExpand all lines: README.rst
+9-38Lines changed: 9 additions & 38 deletions
Display the source diff
Display the rich diff
Original file line number
Diff line number
Diff line change
@@ -24,16 +24,12 @@ The primary component of the SSEBop model is the Image() class. The Image class
24
24
Input Collections
25
25
=================
26
26
27
-
SSEBop ET can currently be computed for Landsat Collection 2 Level 2 (SR/ST) images and Landsat Collection 1 Top-Of-Atmosphere (TOA) images from the following Earth Engine image collections:
27
+
SSEBop ET can currently be computed for Landsat Collection 2 Level 2 (SR/ST) images from the following Earth Engine image collections:
28
28
29
29
* LANDSAT/LC09/C02/T1_L2
30
30
* LANDSAT/LC08/C02/T1_L2
31
31
* LANDSAT/LE07/C02/T1_L2
32
32
* LANDSAT/LT05/C02/T1_L2
33
-
* LANDSAT/LC08/C01/T1_TOA or LANDSAT/LC08/C01/T1_RT_TOA
34
-
* LANDSAT/LE07/C01/T1_TOA or LANDSAT/LE07/C01/T1_RT_TOA
35
-
* LANDSAT/LT05/C01/T1_TOA
36
-
37
33
38
34
**Note:** Users are encouraged to prioritize use of Collection 2 data where available. Collection 1 was produced by USGS until 2022-01-01, and maintained by Earth Engine until 2023-01-01. [`More Information <https://developers.google.com/earth-engine/guides/landsat#landsat-collection-status>`__]
@@ -141,8 +113,6 @@ Land Surface Temperature is currently calculated in the SSEBop approach two ways
141
113
142
114
* Landsat Collection 2 Level-2 (ST band) images directly. More information can be found at: `USGS Landsat Collection 2 Level-2 Science Products <https://www.usgs.gov/core-science-systems/nli/landsat/landsat-collection-2-level-2-science-products>`__
143
115
144
-
* Landsat Collection 1 Top-of-Atmosphere images by including an on-the-fly function for calibration steps and atmospheric correction techniques. These include calculations for: (1) spectral radiance conversion to the at-sensor brightness temperature; (2) atmospheric absorption and re-emission value; and (3) surface emissivity. For additional information, users can refer to section 3.2 of the Methodology in Senay2016_.
145
-
146
116
Temperature Difference (dT)
147
117
---------------------------
148
118
The SSEBop ET model uses dT as a predefined temperature difference between Thot and Tcold for each pixel.
@@ -164,6 +134,7 @@ The 'FANO' parameter (default) can be implemented dynamically for each Landsat s
|Senay, G.B., Parrish, G. E., Schauer, M., Friedrichs, M., Khand, K., Boiko, O., Kagone, S., Dittmeier, R., Arab, S., Ji, L. (2023). Improving the Operational Simplified Surface Energy Balance evapotranspiration model using the Forcing and Normalizing Operation. *Remote Sensing*, 15(1):260.
0 commit comments