Infrared satellite image of Hurricane Katrina approaching south Florida from August 25 at 12:32 PM EDT (1632 UTC). Hurricane tracking maps, current sea temperatures, and more. Risser, M. D. & Wehner, M. F. Attributable human-induced changes in the likelihood and magnitude of the observed extreme precipitation during hurricane … Radar reflectivity image while Katrina was crossing the coast, from August 25 at 6:31 PM EDT (2231 UTC). The 2017 and 2018 Atlantic hurricane seasons set records for precipitation and highlighted the impact hurricanes can have on flooding events in the United States. Keep up with the latest hurricane watches and warnings with AccuWeather's Hurricane Center. Hurricane Katrina was first identified by the NHC as TD 12 at 1800 UTC 23 August 300 km southeast of Nassau, Bahamas. In August 2017 Hurricane Harvey was the wettest storm to flood Texas, and in September 2018 Hurricane Florence set the record for wettest tropical cyclone to impact the … The twenty-first tropical cyclone, eleventh named storm, and seventh hurricane of the 1981 Atlantic hurricane season, Katrina developed from an area of cloudiness in the western Caribbean Sea early on … Hurricane Katrina, tropical cyclone that struck the southeastern United States in August 2005, breaching levees and causing widespread damage and deaths. This is an image of Hurricane Katrina on Sunday, August 28, 2005 at 5:30 PM EDT (21:33 UTC) as seen by the Tropical Rainfall Measuring Mission satellite's PR (Precipitation Radar), VIRS (Visible Infrared Scanner), TMI Read more about Time-Radius Analysis of Hurricane Katrina Satellite Image of Hurricane … Hurricane Katrina was a late-forming tropical cyclone that impacted portions of the Greater Antilles and Bahamas in November 1981. Ultimately, the storm caused more than $160 billion in damage, and it reduced the population of New Orleans by 29 percent between the fall of 2005 and 2011. A time-radius and time-azimuthal distribution of rainfall near Hurricane Katrina. The storm’s initiation followed the WEC pathway described by Davis and Bosart (2004), in which a preexisting lower- to midlevel vortex interacts with a low-latitude upper-level trough to initiate TT.. Each of these features …