![GOES-16 “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/2020/10/atl_vis-20201019_150026.png)
GOES-16 “Red” Visible (0.64 µm) and “Clean” Infrared Window (10.35 µm) images [click to play animation | MP4]
1-minute
Mesoscale Domain Sector GOES-16
(GOES-East) “Red” Visible (
0.64 µm) and “Clean” Infrared Window (
10.35 µm) images
(above) showed Tropical Depression 27 as further intensified to become
Tropical Storm Epsilon at
15 UTC on 19 October 2020. While the low-level circulation (LLC) generally remained exposed during that time, deep convection was increasing around the LLC (including a small convective burst near the storm center forming around 1630 UTC).
![GOES-16 Visible image with plots of available NUCAPS profiles [click to enlarge]](https://cimss.ssec.wisc.edu/satellite-blog/images/2020/10/201019_1640utc_visible_nucapsAvailability.png)
GOES-16 Visible image with plots of available NUCAPS profiles [click to enlarge]
A GOES-16 Visible image with plots of available NOAA-20 NUCAPS profiles
(above) showed one valid infrared (
CrIS) + microwave (
ATMS) sounding
(green dot) just southeast of the center of Epsilon at
1640 UTC — that sounding profile
(below) revealed a moist (PW = 1.95″) and unstable (MU CAPE = 1066 J/kg, and LI = -3) atmosphere just after the time of development of the convective burst near Epsilon’s center.
![NUCAPS profile just southeast of the center of Tropical Storm Epsilon [click to enlarge]](https://cimss.ssec.wisc.edu/satellite-blog/images/2020/10/201019_16utc_nucaps_profile.png)
NUCAPS profile just southeast of the center of Tropical Storm Epsilon [click to enlarge]
GOES-16 Visible images with overlays of
deep-layer wind shear and
GLM Flashes from the
CIMSS Tropical Cyclones site
(below) indicated that Epsilon was in an environment of moderate shear, with limited lighting activity near the storm center.
![GOES-16 “Red” Visible (0.64 µm) images, with overlays of deep-layer wind shear and GLM Flashes [click to enlarge]](https://cimss.ssec.wisc.edu/satellite-blog/images/2020/10/201019_goes16_visible_glm_shear_TS_Epsilon_anim.gif)
GOES-16 “Red” Visible (0.64 µm) images, with overlays of deep-layer wind shear and GLM Flashes [click to enlarge]
A toggle between the
MIMIC Total Precipitable Water and
Saharan Air Layer products
(below) showed that Epsilon was embedded within a pocket of abundant moisture, with dry air situated to the north and northwest.
![MIMIC Total Precipitable Water and Saharan Air Layer product [click to enlarge]](https://cimss.ssec.wisc.edu/satellite-blog/images/2020/10/201019_mimicTPW_SAL_TS_Epsilon_anim.gif)
MIMIC Total Precipitable Water and Saharan Air Layer product [click to enlarge]
Tropical Storm Epsilon was located over water having Sea Surface Temperature values around 28ºC and a modest Ocean Heat Content
(below).
![Sea Surface Temperature and Ocean Heat Content [click to enlarge]](https://cimss.ssec.wisc.edu/satellite-blog/images/2020/10/201019_seaSurfaceTemperature_oceanHeatContent_TS_Epsilon_anim.gif)
Sea Surface Temperature and Ocean Heat Content [click to enlarge]