Tropical Storm Barry
![GOES-16 "Red" Visible (0.64 µm) and "Clean" Infrared Window (10.35 µm) images, with plots of buoy and ship reports [click to play MP4 animation]](https://cimss.ssec.wisc.edu/satellite-blog/wp-content/uploads/sites/5/2019/07/barry_vis-20190711_150110.png)
GOES-16 “Red” Visible (0.64 µm) and “Clean” Infrared Window (10.35 µm) images, with plots of buoy and ship reports [click to play MP4 animation]
As was seen in an animation of GOES-16 Infrared imagery from the CIMSS Tropical Cyclones site (below), Barry was in an environment of low deep-layer wind shear — a factor that was favorable for further intensification.
===== 12 July Update =====

GOES-16 “Red” Visible (0.64 µm) images [click to play animation | MP4]
The corresponding GOES-16 Infrared images (below) showed that deep convection remained to the south of the center of Barry.
![GOES-16 "Clean" Infrared Window (10.35 µm) images [click to play animation | MP4]](https://cimss.ssec.wisc.edu/satellite-blog/wp-content/uploads/sites/5/2019/07/barry_ir-20190712_171710.png)
GOES-16 “Clean” Infrared Window (10.35 µm) images [click to play animation | MP4]
===== 17 July Update =====
An Aqua MODIS Sea Surface Temperature image 2 days prior to the formation of Tropical Storm Barry (above) showed SST values in the upper 80s to low 90s F (darker shades of orange to red) in the northern Gulf of Mexico just south of Louisiana.8 days later, a Terra MODIS SST image (below) revealed values predominantly in the lower to middle 80s F (green to yellow enhancement) — the slow movement of Barry as it eventually reached hurricane intensity just prior to landfall induced an upwelling of cooler sub-surface water over that area.