• DocumentCode
    161913
  • Title

    The role of regional-scale ocean observations for improved hurricane intensity and impact forecasts in coastal regions

  • Author

    Glenn, Scott ; Seroka, Greg ; Miles, Travis ; Yi Xu ; Roarty, Hugh ; Kohut, Josh ; Schofield, Oscar

  • Author_Institution
    Rutgers Univ., New Brunswick, NJ, USA
  • fYear
    2014
  • fDate
    7-10 April 2014
  • Firstpage
    1
  • Lastpage
    9
  • Abstract
    The coastal northeast United States was heavily impacted by hurricanes Irene and Sandy. Track forecasts for both hurricanes were quite accurate days in advance. Intensity forecasts, however, were less accurate, with the intensity of Irene significantly over-predicted, and the rapid acceleration and intensification of Sandy just before landfall under-predicted. By operating a regional component of the Integrated Ocean Observing System (IOOS), we observed each hurricane´s impact on the ocean in real-time, and we studied the impacted ocean´s influence on each hurricane´s intensity. Summertime conditions on the wide Mid-Atlantic continental shelf consist of a stratified water column with a thin (10m-20m) warm surface layer (24-26C) covering bottom Cold Pool water (8-10C). As the leading edge of the Irene tracked along the coast, real-time temperature profiles from an underwater glider documented the mixing and broadening of the thermocline that rapidly cooled the surface by up to 8 C, well before the eye passed over. Atmospheric forecast sensitivity studies indicate that the over prediction of intensity in Irene could be reduced using the observed colder surface waters. In contrast, Hurricane Sandy arrived in the late Fall of 2012 after seasonal cooling had already deepened and decreased surface layer ocean temperatures by 8C. The thinner layer of cold bottom water still remaining before Sandy was forced offshore by downwelling favorable winds, resulting in little change in ocean surface temperature as Sandy crossed and mixed the shelf waters. Atmospheric sensitivity studies indicate that because there was little ocean cooling, there was little reduction in hurricane intensity as Sandy came ashore. Results from Irene and Sandy illustrate the important role of the U.S. IOOS in providing the best estimate of the rapidly evolving ocean conditions to atmospheric modelers forecasting the intensity of hurricanes. Data from IOOS may enable improved hurricane forecasting in- the future.
  • Keywords
    mixing; ocean temperature; storms; weather forecasting; wind; AD 2012; IOOS data; IOOS regional component; Integrated Ocean Observing System; Intensity forecast; Irene intensity over-prediction; Irene intensity prediction; Irene tracked leading edge; Mid-Atlantic continental shelf; Sandy intensification; US IOOS; atmospheric forecast sensitivity; atmospheric modeler forecasting; bottom cold pool water; coastal northeast United States; coastal region; crossed shelf water; decreased surface layer ocean temperature; deepened surface layer ocean temperature; downwelling favorable wind; hurricane Irene; hurricane Sandy; hurricane intensity reduction; hurricane track forecast; impacted ocean; improved hurricane forecasting; improved hurricane impact forecast; improved hurricane intensity; landfall under-prediction; mixed shelf water; observed colder surface water; ocean cooling; ocean surface temperature; rapid Sandy acceleration; rapidly cooled surface; rapidly evolving ocean condition estimation; real-time hurricane ocean impact; real-time temperature profile; regional-scale ocean observation; seasonal cooling; stratified water column; summertime condition; thermocline broadening; thermocline mixing; thinner cold bottom water layer; underwater glider; warm surface layer; Atmospheric modeling; Hurricanes; Ocean temperature; Radar tracking; Sea surface; Storms; Atmospheric Modeling; HF Radar; Hurricane Forecasting; Ocean Modeling; U.S. IOOS; Underwater Gliders;
  • fLanguage
    English
  • Publisher
    ieee
  • Conference_Titel
    OCEANS 2014 - TAIPEI
  • Conference_Location
    Taipei
  • Print_ISBN
    978-1-4799-3645-8
  • Type

    conf

  • DOI
    10.1109/OCEANS-TAIPEI.2014.6964331
  • Filename
    6964331