1-minute Mesoscale Domain Sector GOES-17 (GOES-West) “Red” Visible (0.64 µm) images (above) showed the convective banding associated with Tropical Invest 90E in the East Pacific Ocean on 08 May 2021. Invest 90E was centered along a northward bulge in the ITCZ/Monsoon Trough (below).Invest 90E was located over water characterized by modest Ocean Heat Content and very... Read More
![GOES-17 “Red” Visible (0.64 µm) and "Clean" Infrared Window images [click to play animation | MP4]](https://cimss.ssec.wisc.edu/satellite-blog/images/2021/05/90e_vis-20210508_180059.png)
GOES-17 “Red” Visible (0.64 µm) and “Clean” Infrared Window (10.35 µm) images [click to play animation | MP4]
1-minute
Mesoscale Domain Sector GOES-17
(GOES-West) “Red” Visible (
0.64 µm) images
(above) showed the convective banding associated with Tropical Invest 90E in the East Pacific Ocean on 08 May 2021. Invest 90E was centered along a northward bulge in the
ITCZ/Monsoon Trough
(below).

GOES-17 “Clean” Infrared Window (10.35 µm) image (Mesoscale Sector), with an overlay of the 12 UTC surface analysis [click to enlarge]
Invest 90E was located over water characterized by modest Ocean Heat Content and very warm Sea Surface Temperature values
(below), favorable factors for further intensification.
![Ocean Heat Content and Sea Surface Temperature [click to enlarge]](https://cimss.ssec.wisc.edu/satellite-blog/images/2021/05/210508_oceanHeatContent_seaSurfaceTemperature_Invest90E_anim.gif)
Ocean Heat Content and Sea Surface Temperature [click to enlarge]
===== 09 May Update =====
![GOES-17 “Red” Visible (0.64 µm) and "Clean" Infrared Window (10.35 µm) images [click to play animation | MP4]](https://cimss.ssec.wisc.edu/satellite-blog/images/2021/05/one_ir-20210509_150059.png)
GOES-17 “Red” Visible (0.64 µm) and “Clean” Infrared Window (10.35 µm) images [click to play animation | MP4]
1-minute GOES-17 Infrared and Visible images on 09 May
(above) showed the period where Invest 90E intensified to a Tropical Depression (at 0900 UTC) and then to
Tropical Storm Andres at 1500 UTC — the earliest calendar year tropical storm on record in the East Pacific basin. The convective overshooting tops occasionally exhibited infrared brightness temperatures of -90ºC or colder
(yellow pixels embedded within dark purple regions).
A GOES-17 Infrared / Water Vapor Difference product (reference) from the CIMSS Tropical Cyclones site (below) highlighted areas of deep convection where overshooting tops were likely penetrating the tropopause (yellow to red enhancement).
![GOES-17 Infrared - Water Vapor Difference product [click to enlarge]](https://cimss.ssec.wisc.edu/satellite-blog/images/2021/05/210509_goes17_irwvdiff_TS_Andres_anim.gif)
GOES-17 Infrared – Water Vapor Difference product [click to enlarge]
GOES-17 Infrared images, with an overlay of
deep-layer wind shear (below) indicated that Andres was approaching an environment of moderate to high shear, which would limit intensification.
![GOES-17 Infrared images, with an overlay of deep-layer wind shear [click to enlarge]](https://cimss.ssec.wisc.edu/satellite-blog/images/2021/05/210509_goes17_infrared_shear_TS_Andres_anim.gif)
GOES-17 Infrared images, with an overlay of deep-layer wind shear [click to enlarge]
===== 10 May Update =====
![GOES-17 “Red” Visible (0.64 µm) and "Clean" Infrared Window (10.35 µm) images [click to play animation | MP4]](https://cimss.ssec.wisc.edu/satellite-blog/images/2021/05/ts_vis-20210510_214755.png)
GOES-17 “Red” Visible (0.64 µm) and “Clean” Infrared Window (10.35 µm) images [click to play animation | MP4]
On 10 May, 1-minute GOES-17
Infrared and Visible images (above) showed that after one final convective burst, the low-level center of Tropical Storm Andres became exposed — and the storm was then downgraded to a Tropical Depression at 2100 UTC.
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