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Published byMuriel Houston Modified over 8 years ago
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Arc Clouds in the Tropical Cyclone Environment Jason P. Dunion 1, Jeff Hawkins 2, and Chris Velden 3 1 NOAA/AOML/Hurricane Research Division 2 NRL-Monterey 3 UW-CIMSS
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Discussion Outline Motivation Background - new mean soundings for the tropical NATL Arc Clouds - Midwest t - storms vs TCs - hypotheses (TCs) - arc clouds & TCs Future Work Conclusions
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Motivation How does moisture and vertical wind shear in the surrounding TC environment impact TC intensity? …and where do arc clouds fit in to all this?
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Miami Swan Island San Juan, Grand Cayman Guadeloupe The Jordan Mean Tropical Sounding (1958) 10 yr dataset (1946-1955) Averaged over the months of the “hurricane season”: July-Oct 1995-2002 ( July-October) 6,000 Caribbean rawinsondes 3,000 GOES images processed
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New Mean Moisture Soundings Moist Tropical, SAL, and Mid-latitude dry air intrusions
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Arc Clouds …aka Arcus Clouds (Roll Cloud; Shelf Cloud) Arc Clouds
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Midwest T-storm Tropical Cyclone Duration ~30 min~5 days (named) Size ~15 mi ~300-400 mi *TCs have to stick it out in their environment* Motion ~25-30 kt ~10-12 kt Arc Clouds: Thunderstorms vs TCs Downdrafts lead to dissipation phase disruption to the system
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Arc Clouds Hypotheses 1. The moist tropical sounding is insufficiently dry in the mid- levels to form substantial arc clouds 2. Arc clouds inhibit TC development in the short term by: a) promoting downdrafts locally b) promoting low to mid-level outflow c) bringing cool, dry air down into the boundary layer
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Shear: 10kt @5 Shear (12z): 15kt @258 Shear (18z): 23kt @243 16 Sept 1740 UTC Hurricane Isabel: September 2003 All 3 new soundings: ~95-96% of column moisture is below 500 hPa TPW: MT=51.5 mm; SAL=40mm; MLDAI=36 mm
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14 Sep 2007 1127 UTC 14 Sep 2007 1632 UTC Tropical Storm Ingrid 14 Sept 2007
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Arc Clouds (cont’d) Felix ‘07 Vertical Shear T(-24): 285/11 kt T(0): 280/15 kt Low to Moderate Westerly Vertical Shear T(-24): 140/11 kt T(0): 331/6 kt kt SE to NNW Fabian ‘03
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Arc Clouds (cont’d) Paloma ‘08 Vertical Shear T(-24): 156/2 kt T(0): 219/12 kt SSE to SW
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Tropical Storm Dolly: 21 July 2008 G-IV Synoptic Surveillance Mission 080721N Photo credit: Paul Flaherty NOAA/AOC
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Hunting for Arc Clouds Arc Clouds Arc Cloud
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Simple Cloud Model (DeMaria): MT/SAL/MLDAI Parcel initialized at z=0 with a 10 m/s updraft (r=500 m) Parcel entrains environmental air along the way Entrainment coeff= 0.1 Height (km)
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Conclusions Future Work -Conduct HRD’s Arc Cloud module (P-3s, G-IV, Aerosonde) a) arc cloud-TC relationship b) shear-dry air impacts on TCs (tag team effect) -Continue modeling studies using these 3 new soundings New mean soundings (tropical NATL & Caribbean) -Moist Tropical, SAL, and MLDAI -Distinguishing MT from SAL & MLDAI: 45 mm TPW Arc Clouds -Different implications: Midwest t-storms vs TCs -MT sounding: insufficiently mid-level dryness to form arc clouds -Disruption of TC via: a) promoting downdrafts locally b) promoting low to mid-level outflow c) bringing cool, dry air down into the boundary layer
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