By Scott Lindstrom •
The 2016 Atlantic Tropical Season’s third named storm has formed in the Gulf of Mexico just north of the Yucatan Peninsula; Colin became the earliest named “C” storm on record for that basin. MIMIC Total Precipitable Water values for the 72 hours ending at 2300 UTC on 5 June 2016, above, show the storm embedded within a deep band of tropical moisture that has surged northward from the Monsoon Trough / Intertropical Convergence Zone into the northwestern Caribbean and southern Gulf of Mexico (MIMIC TPW + surface analyses). Moisture extends northeastward along the projected path of the storm into northern Florida. Extensive rains are likely over the Southeast US as the storm moves north. Total Precipitable Water (TPW) from MIMIC is a simple band difference between two microwave channels; that difference is invalid over land where emissivity is highly variable. However, MIRS data can estimate TPW over land and water, and its distribution over the eastern United States, below, derived from a morphed animation of the observations, gives a better indication of the spread of rich moisture over the southeastern United States. In addition, the Blended TPW Product showed values in excess of 70 mm (2.76 inches) over the Gulf of Mexico, which were in excess of 170% of Normal. Colin was poised to moved over a region of higher Ocean Heat Content that was located in the eastern Gulf of Mexico, which could help to fuel additional bursts of deep convection similar to that seen on POES AVHRR infrared imagery, below. For more information on Tropical Storm Colin, refer to the CIMSS Tropical Cyclones site and the National Hurricane Center.Categories: Aqua, AVHRR, DMSP, Metop, POES, Tropical cyclones