Jump to content
  • Member Statistics

    17,587
    Total Members
    7,904
    Most Online
    LopezElliana
    Newest Member
    LopezElliana
    Joined

Hurricane Sandy thread


usedtobe

Recommended Posts

IN ADDITION...HURRICANE-FORCE WINDS ARE EXPECTED ALONG PORTIONS OF

THE COAST BETWEEN CHINCOTEAGUE VIRGINIA AND CHATHAM MASSACHUSETTS.

THIS INCLUDES THE TIDAL POTOMAC FROM COBB ISLAND TO SMITH POINT...

THE MIDDLE AND UPPER CHESAPEAKE BAY...DELAWARE BAY...AND THE COASTS

OF THE NORTHERN DELMARVA PENINSULA...NEW JERSEY...THE NEW YORK CITY

AREA...LONG ISLAND...CONNECTICUT...AND RHODE ISLAND.

I live 5 miles from the Bay, and my girl lives on the water, we're gonna the best gusts, 70-80mph

Link to comment
Share on other sites

  • Replies 640
  • Created
  • Last Reply

This is the lower half of the Tidal Potomac FYI... upper half still Storm Warning

URGENT - MARINE WEATHER MESSAGE

NATIONAL WEATHER SERVICE BALTIMORE MD/WASHINGTON DC

501 PM EDT SUN OCT 28 2012

ANZ537-290515-

/O.UPG.KLWX.SR.W.0001.000000T0000Z-121031T0000Z/

/O.EXA.KLWX.HF.W.0001.000000T0000Z-121031T0000Z/

TIDAL POTOMAC FROM COBB ISLAND MD TO SMITH POINT VA-

501 PM EDT SUN OCT 28 2012

...HURRICANE FORCE WIND WARNING IN EFFECT UNTIL 8 PM EDT

TUESDAY...

THE NATIONAL WEATHER SERVICE IN STERLING VIRGINIA HAS ISSUED A

HURRICANE FORCE WIND WARNING...WHICH IS IN EFFECT UNTIL 8 PM EDT

TUESDAY. THE STORM WARNING IS NO LONGER IN EFFECT.

* WINDS...64 KNOTS OR GREATER WITHIN THE HURRICANE FORCE WIND

WARNING. 48 TO 63 KNOTS WITHIN THE STORM WARNING.

Link to comment
Share on other sites

LWX again ramping up... though 60-70 arent hurricane force...

URGENT - WEATHER MESSAGE

NATIONAL WEATHER SERVICE BALTIMORE MD/WASHINGTON DC

501 PM EDT SUN OCT 28 2012

...THE NATIONAL HURRICANE CENTER FORECASTS HURRICANE SANDY TO

TRACK TO THE NORTHEAST TO A POSITION WELL OFF THE NORTH CAROLINA

COAST TONIGHT...BEFORE SHIFTING TO THE NORTHWEST AND MOVING

TOWARD NEW JERSEY MONDAY INTO TUESDAY. THE TRACK OF SANDY IS

EXPECTED TO BRING HIGH WINDS TO THE REGION MONDAY MORNING THROUGH

TUESDAY EVENING...

DCZ001-MDZ004>007-009>011-013-014-016>018-VAZ053-054-290515-

/O.CON.KLWX.HW.W.0002.121029T1200Z-121031T0000Z/

DISTRICT OF COLUMBIA-FREDERICK MD-CARROLL-NORTHERN BALTIMORE-

HARFORD-MONTGOMERY-HOWARD-SOUTHERN BALTIMORE-PRINCE GEORGES-

ANNE ARUNDEL-CHARLES-ST. MARYS-CALVERT-FAIRFAX-

ARLINGTON/FALLS CHURCH/ALEXANDRIA-

INCLUDING THE CITIES OF...WASHINGTON...FREDERICK...WESTMINSTER...

GAITHERSBURG...COLUMBIA...BALTIMORE...ANNAPOLIS...WALDORF...

ST MARYS CITY...FAIRFAX...ALEXANDRIA...FALLS CHURCH

501 PM EDT SUN OCT 28 2012

...HIGH WIND WARNING REMAINS IN EFFECT FROM 8 AM MONDAY TO 8 PM

EDT TUESDAY...

* TIMING...SUSTAINED WINDS OF 30 TO 40 MPH ARE EXPECTED BY 8 AM

MONDAY...THEN INCREASING AROUND NOONTIME MONDAY TO 35 TO 45 MPH

WITH HURRICANE FORCE WIND GUSTS 60 TO 70 MPH LASTING INTO EARLY

TUESDAY MORNING.

* IMPACTS...A PROLONGED AND SIGNIFICANT 24 HOUR HIGH WIND EVENT

WILL TAKE PLACE ACROSS THE WARNING AREA. COUPLED WITH HEAVY

RAINS FROM SANDY...THE HIGH WINDS WILL LEAD TO SIGNIFICANT TREE

DAMAGE. RESIDENTS...VISITORS... AND BUSINESSES ACROSS THE REGION

SHOULD PLAN FOR WIDESPREAD POWER AND COMMUNICATION OUTAGES.

Link to comment
Share on other sites

* TIMING...SUSTAINED WINDS OF 30 TO 40 MPH ARE EXPECTED BY 8 AM

MONDAY...THEN INCREASING AROUND NOONTIME MONDAY TO 35 TO 45 MPH

WITH HURRICANE FORCE WIND GUSTS 60 TO 70 MPH LASTING INTO EARLY

TUESDAY MORNING.

yeah they were conservative early probably in case it shifted as there is a fairly steep gradient from the strongest to just strong to our sw.

Link to comment
Share on other sites

Can someone explain model SLP initialization? 18z nam shows 968 @ init. 12z gfs showed 972. Why is this?

I'm sure there is a reason but pressures just seem way off. 18z nam shows 960'ish at landfall. Wouldn't we expect 950'ish at this point? Even mid 940's seem more likely than 960.

Link to comment
Share on other sites

Can someone explain model SLP initialization? 18z nam shows 968 @ init. 12z gfs showed 972. Why is this?

I'm sure there is a reason but pressures just seem way off. 18z nam shows 960'ish at landfall. Wouldn't we expect 950'ish at this point? Even mid 940's seem more likely than 960.

I can't explain it but I know deep tropical systems are almost always initialized too weak.

Link to comment
Share on other sites

Can someone explain model SLP initialization? 18z nam shows 968 @ init. 12z gfs showed 972. Why is this?

I'm sure there is a reason but pressures just seem way off. 18z nam shows 960'ish at landfall. Wouldn't we expect 950'ish at this point? Even mid 940's seem more likely than 960.

See posts 262 and 265:

http://www.americanwx.com/bb/index.php/topic/37397-hurricane-sandy-model-and-medium-range-discussion/page__st__245

Link to comment
Share on other sites

Can someone explain model SLP initialization? 18z nam shows 968 @ init. 12z gfs showed 972. Why is this?

I'm sure there is a reason but pressures just seem way off. 18z nam shows 960'ish at landfall. Wouldn't we expect 950'ish at this point? Even mid 940's seem more likely than 960.

I just read a post by dtk in the general forum that explained it.

Link to comment
Share on other sites

Can someone explain model SLP initialization? 18z nam shows 968 @ init. 12z gfs showed 972. Why is this?

I'm sure there is a reason but pressures just seem way off. 18z nam shows 960'ish at landfall. Wouldn't we expect 950'ish at this point? Even mid 940's seem more likely than 960.

I have a follow up to a post that Phil made in the main tropical modeling thread. It basically has to do with representativeness (i.e. they are intentionally given initial conditions that do not result in significant spin-down issues).... The NAM uses very little data in the vicinity of TCs (no bogusing, no relocation, etc.). The GFS does draw toward the NHC issues advisory SLP, but conservatively so (I have a paper on this if people are interested).

There is also an issue of post processing (the SLP field that is plotted is not actually from the model...it is interpoloated and smoothed, at least for the GFS). I am hoping that we can convince people to start using the non-smoothed (alternative extrapolation) version of SLP (which already exists in our grib files) for the GFS.

Link to comment
Share on other sites

I have a follow up to a post that Phil made in the main tropical modeling thread. It basically has to do with representativeness (i.e. they are intentionally given initial conditions that do not result in significant spin-down issues).... The NAM uses very little data in the vicinity of TCs (no bogusing, no relocation, etc.). The GFS does draw toward the NHC issues advisory SLP, but conservatively so (I have a paper on this if people are interested).

There is also an issue of post processing (the SLP field that is plotted is not actually from the model...it is interpoloated and smoothed, at least for the GFS). I am hoping that we can convince people to start using the non-smoothed (alternative extrapolation) version of SLP (which already exists in our grib files) for the GFS.

I'm glad you answered, I started to but you know more about the subject than I do.

Link to comment
Share on other sites

I'm glad you answered, I started to but you know more about the subject than I do.

Wes, your comment about smoothing is also a good one. The estimated minimum SLP from NHC is a point measurement, not something we can simply drop into the model. The net effect of the assimilation is to take that information and smooth it out (typicall with reduced amplitude). Furthermore, observations have errors too, so we cannot statistically assume that the observation is ground truth (hence it is combined with the model state through the assimilation process).

People really need to be careful NOT to use the initialized minimum SLP for a reason as to whether or not to use model A over model B. The hurricane models (HWRF, GFDL) generally use various initialization and or bogusing techniques to attempt to put in vortices as close to the observations as possible (but again, those model's inner domains are explicitly designed to forecasts TCs).

Link to comment
Share on other sites

Thanks all for the excellent explanations. Does the same pressure differences in the solutions change anything irt sensible wx at the surface? Doesn't look like it to me but I'm far from an expert on this stuff.

Edit: I want to add one more question that seems important. If the GFS / NAM show the pressure dropping 10+/- mb between init and lf, can we assume the same 10mb drop from where we are now? A 940mb LF is quite concerning but I'm not sure expecting something like that is realistic.

Link to comment
Share on other sites

It looks pretty darn good this afternoon.. inner core has rebuilt a good bit. I wonder what happens if it doesn't ET transition fully. I won't join on the NHC bashing but it is weird to have "the biggest storm ever" and no warnings from them north of NC. Will we be able to call it the great hurricane of 2012?

post-1615-0-99450400-1351454913_thumb.jp

That picture is simply amazing. Absolutely huge storm. Has anyone ever seen a hurricane hit the N/E with that kind of size?

Link to comment
Share on other sites

Wes, your comment about smoothing is also a good one. The estimated minimum SLP from NHC is a point measurement, not something we can simply drop into the model. The net effect of the assimilation is to take that information and smooth it out (typicall with reduced amplitude). Furthermore, observations have errors too, so we cannot statistically assume that the observation is ground truth (hence it is combined with the model state through the assimilation process).

People really need to be careful NOT to use the initialized minimum SLP for a reason as to whether or not to use model A over model B. The hurricane models (HWRF, GFDL) generally use various initialization and or bogusing techniques to attempt to put in vortices as close to the observations as possible (but again, those model's inner domains are explicitly designed to forecasts TCs).

Daryl, I deleted my post after you made yours but I agree that people need to be real careful about blowing off a solution based on having too weak a surface low.

Link to comment
Share on other sites

Archived

This topic is now archived and is closed to further replies.

  • Recently Browsing   0 members

    • No registered users viewing this page.

×
×
  • Create New...