Band 2 is a bit less eye-candyish but you can really see the mackeralling. I wonder why that is. I assume that there is enough friction between the layers for the over running high speed layer to scuff up waves on the surface of the underlying layer and if the underlying layer is moisture-critical, we will see mackeralling of the clouds (ie; Alto cumulus streets.) Thanks for sending it.
n Nick Thompson <mailto:[email protected]> [email protected] <https://wordpress.clarku.edu/nthompson/> https://wordpress.clarku.edu/nthompson/ From: Friam <[email protected]> On Behalf Of Marcus Daniels Sent: Thursday, December 9, 2021 1:19 PM To: The Friday Morning Applied Complexity Coffee Group <[email protected]> Subject: Re: [FRIAM] GOES-East - Sector view: Southern Rockies - Band 2 - NOAA / NESDIS / STAR https://arstechnica.com/science/2021/12/revisiting-the-tsar-bomba-nuclear-te st/ From: Friam <[email protected] <mailto:[email protected]> > On Behalf Of [email protected] <mailto:[email protected]> Sent: Thursday, December 9, 2021 10:30 AM To: 'The Friday Morning Applied Complexity Coffee Group' <[email protected] <mailto:[email protected]> > Subject: [FRIAM] GOES-East - Sector view: Southern Rockies - Band 2 - NOAA / NESDIS / STAR https://www.star.nesdis.noaa.gov/GOES/sector_band.php?sat=G16 <https://www.star.nesdis.noaa.gov/GOES/sector_band.php?sat=G16§or=sr&ban d=02&length=24> §or=sr&band=02&length=24 "Layers of the atmosphere do not mix."
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