OCEANIC AND ATMOSPHERIC MEASUREMENTS IN HURRICANES ISIDORE AND LILI (2002) - PowerPoint PPT Presentation

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OCEANIC AND ATMOSPHERIC MEASUREMENTS IN HURRICANES ISIDORE AND LILI (2002)

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oceanic and atmospheric measurements in hurricanes isidore and lili (2002) mpo, rsmas, univ. of miami nsf atm-01-08218, noaa jht – PowerPoint PPT presentation

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Title: OCEANIC AND ATMOSPHERIC MEASUREMENTS IN HURRICANES ISIDORE AND LILI (2002)


1
OCEANIC AND ATMOSPHERIC MEASUREMENTS IN
HURRICANES ISIDORE AND LILI (2002)
  • MPO, RSMAS, Univ. of Miami
  • NSF ATM-01-08218,
  • NOAA JHT

2
Acknowledgments
  • Capt. Bob Maxson and Dr. Jim McFadden (AOC) and
    the entire staff (pilots, engineers,
    technicians).
  • Dr. Frank Marks (NOAA-HRD) for his continued
    support and HRD staff.
  • Dr. Steve Nelson (NSF-Dynamic Mesoscale
    Meteorology Program) for his continued support.
  • Dr. Russell Elsberry and the USWRP for
    recognizing the importance of the upper ocean on
    TC intensity issues.
  • Mr. Tom Cook and Dr. S. Daniel Jacob (UMBC)
  • Mr. Eric Uhlhorn, Cmdr. Sean White, Mr. Scott
    Guhin, Mr. Mike McGauley, Mr. Mike Black, and Mr.
    Robbie Berg.

3
Introduction
  • Long-term goal of the research is to understand
    the role of the upper ocean on hurricane
    intensity changes.
  • Oceanic Heat Content (based on seasonal
    climatology and radar altimetry) improves
    predictive intensity models (i.e. SHIPS)-now part
    of the operational data stream (DeMaria et al.
    2002, 2004 Mainelli et al. 2002 Mainelli and
    Shay 2004).
  • Not the full story-OHC is modulated by vertical
    mixing processes through vertical current shear.
    Since 84, Only 6 Storms where Vertical Current
    Shear has been measured from AXCPs.
  • Overview of Isidore and Lili data set acquired
    from AXCPs and AXCTDs and the GPS sondes prior,
    during and subsequent to their passage in the
    Gulf of Mexico.
  • Relevant to modeling here at NCEP.

4
Challenge Getting the current and shear
correct in models for mixing.
5
Conceptual Model GOM
6
SST Response
7
Oceanic Heat Content Relative to 26C
8
2002 Summary Isidore and Lili
GPS/AXBT/AXCP/AXCTDs From 42/43
9
Hurricane Isidore Pre-Storm, Storm,
Post-StormAXCP/AXCTD/AXBTs
10
Hurricane Isidore Radar and Scatterometer
11
SST (left panels) and OHC (right panels) for
Pre-Isidore (upper) and Post-Isiidore
(lower) Relative to Storm Intensity. (SSTs
processed by RSMAS Remote Sensing Laboratory).
12
Pre-Post Isidore SST and OHC
13
Hurricane Lili Pre-Storm, Storm,
Post-StormAXCP/AXCTD/AXBTs
14
Hurricane Lili Radar and Scatterometer
15
43 Lili In Storm Gulf of MexicoRapid Deepening
Cycle!
16
SST (left panels) and OHC (right panels) for
Pre-Lili (upper) and Post-Lili (lower) Relative
to Storm Intensity. (SSTs processed by RSMAS
Remote Sensing Laboratory).
17
Buoy 42001 Measurements(from White and Shay 2004)
18
GPS sondes During the Lilis Relative to
Intensity and Track. G-IV (Left panel), P-3
(Right panels)
19
Theta_e/Wind Variability at 24N
20
Pre-Post Lili SST and OHC
21
Hurricane Lili Post-Storm AXCP Transect at 2Rmax
22
Lilis Wind Field from HWIND Relative To
Gridded Domain
23
Pre-Storm OHC and Depth of 26oC Isotherm
24
Pre- and Post OML Temperatures
25
Post-Storm OML and Thermocline Currents
26
Normalized OHC Change Versus Shear2 Production
27
Hurricane Lili 2 Oct 02
28
Hurricane Lili 2 Oct 02 Fluxes
29
Pre-Storm OHC Satellite and In Situ Measurements
30
Ocean Profiles From EPAC, GOM, and LC based on
AXCTDs.
31
Challenge Fully Coupled Ocean Atmosphere
Model
32
Comparison of Mixing Schemes in HYCOM During
the Passage of Gilbert.
33
HYCOM
  • North Atlantic HYCOM at 0.08 resolution
    extending from 28 S to 70 N. 26 levels/ layers
    in the vertical.
  • High resolution surface forcing from FNMOC with
    Salinity relaxation at the surface.
  • 3 buffer zones in the north and south relaxed
    to climatology.
  • Satellite altimeter surface height anomalies from
    the MODAS operational system at NAVOCEANO
    (Initial Fields Are Important!).
  • Mean Sea Surface Height from the 0.08 Atlantic
    MICOM.
  • Vertical projection of surface height signature
    using the Cooper-Haines (1996) technique.
  • Sea Surface Temperature not assimilated at
    present.

34
Summary
  • Best Ocean-Atmosphere Data Set Ever Acquired
    During TC Passage!
  • Successful set of experiments due to the teamwork
    between NSF and NOAA-unique opportunity during a
    rapid deepening cycle.
  • Vertical current shear modulates SST/OHC
    variability and heat fluxes, and must be measured
    more frequently (T(z) is NOT enough).
  • Improve satellite algorithms for OHC/SHIPS
    Forecasting of TC and Oceanic component of models
    at Operational Centers (NCEP).
  • Data set will contribute to several MS/PhD
    studies (Uhlhorn, White, Guhin, McGauley).
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