![\"GOES-16](\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2018\/07\/180713_goes16_visible_ex_Beryl_anim.gif\")
<\/a>GOES-16 “Red” Visible (0.64 \u00b5m)<\/em> images [click to play animation]<\/p><\/div>GOES-16 (GOES-East)<\/em> “Red” Visible (0.64 \u00b5m<\/strong><\/a>) images (above)<\/strong><\/em> depicted the remnants of Hurricane Beryl<\/strong><\/a>, which was situated off the East Coast of the US on 13 July 2018. Note the presence of 2 apparent low-level circulation centers — the primary circulation became better exposed as areas of deep convection moved more quickly to the east.<\/p>\n Overlays of low-level (produced using Visible Band 2)<\/em> and upper-level (produced using Water Vapor Band 8)<\/em> Derived Motion Winds (below)<\/strong><\/em> highlighted the primary low-level circulation, as well as the trough aloft whose axis was located just to the west.<\/p>\n GOES-16 “Red” Visible (0.64 \u00b5m)<\/em> images, with low-level (Visible Band 2)<\/em> Derived Motion Winds plotted in yellow and upper-level (Water Vapor Band 8)<\/em> Derived Motion Winds plotted in cyan [click to play animation]<\/p><\/div>Contours of Deep-Layer Wind Shear from the CIMSS Tropical Cyclones<\/strong><\/a> site (below)<\/strong><\/em> revealed that there was a large gradient in shear over the region at 19 UTC, with higher shear northwest of the system — this verified the subjective appearance of high shear in that particular area, where low-level and upper-level Derived Motion Winds were nearly orthogonal.<\/p>\n<\/a>