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LST_cci User Workshop 2020 - Shared screen with speaker view
Lizzie Good
06:07:21
Padlet link for this land-atmosphere interaction session is https://padlet.com/infolstcci/2xxeihiso3ut2e59
Alejandro DUSSAILLANT (UK/Chile)
06:13:09
@Roel: what air temperature do you compare with LST? How near the surface and how do you measure it (sampling "control volume" and how do you account for interference from sensor temperature)?
Clement Albergel (ESA)
06:15:04
@Roel: on the GPP for the cropland site, is it harvesting you see in the in-situ measurements but not in the retrieval? Or did I miss something?
Alejandro DUSSAILLANT (UK/Chile)
06:18:51
thanx Roel
Clement Albergel (ESA)
06:20:28
Thanks Roel!
Annu Panwar
06:35:57
Very interesting study, Specially the use of LST and SST to better understand land-sea breeze. I would like to know what explains the phase differences you showed for wind, temperature gradient diurnal cycles. Is it something standard (~5 degrees celcius of thermal gradient) or it may vary ecosystem to ecosystem?
Taylor, Christopher M.
06:36:04
Interesting sea breeze characterisation. Did you sea reduced LST and sea breezes in the days after heavy rain, when evaporation is more important?
Joao Martins
06:36:13
I have a question!
Annu Panwar
06:37:45
Thanks ! Catch you in padlet
Habtamu tsegaye
06:56:25
how can you compare your result with other literature with different season?
Taylor, Christopher M.
06:57:26
Are the night-time LSTs in the Sahel sensitive to the presence of high water vapour in the atmosphere modulating down-welling LW at the surface? I know that this effect is important for air temperature variability during MAM in the Sahel
Annu Panwar
06:57:31
Can you quantify, by how much temperature decreases with an increase in unit soil moisture? Why not look at air temperature. Also, How do you correct for the contribution of solar radiation on LST, which varies with latitudes. I work on similar objectives. I find vegetation very important to consider.