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WxUSAF

Moderator Meteorologist
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Posts posted by WxUSAF

  1. Been repainting my deck for the last five week. Finally have one full coat on it. Previous owners did a sh-tty job when they did it so the deck was peeling and two colors. Looks much better now. 

    And as always trying to get grass to grow in bare spots. This weekends 0.03” of rain didn’t help much.

  2. 13 hours ago, gymengineer said:

    Wait, how did it accumulate on streets here and not where you are? 

    See the photos from Wheaton and Savage:

    https://www.washingtonpost.com/amphtml/news/capital-weather-gang/wp/2013/03/25/beautiful-spring-snow-blankets-washington-d-c-area/

    I'm pretty sure Matt has posted pics of snow on paved surfaces in DC that early morning too.

    Maybe it did and I just forgot. But I remember having no issues driving to work.

  3. 2 minutes ago, gymengineer said:

    And I will still enjoy that 3" slop storm. :) I have very pleasant memories of 3/24-25/13.

    My jumping date is 4/7 in any winter-- the end date of the last ground covering snow in my lifetime. (1990- 3.8" at IAD)

    I thought 3/25/13 was ridiculous. I had ~6", nothing on the streets, didn't even get a day off work, and it was all gone by lunch.  

    • Like 1
  4. 10 below normal months at BWI in the period of November 13-February 15. 

     

    February 15, January 15, November 14, August 14, July 14, April 14, March 14, February 14, January 14, November 13

     

    That's a pretty impressive run given climate and UHI both progressively working against below normal temps.  Maybe some of the stat-minded folks can tell us how exceptional it is?

  5. Record high warning being issued for Sunday at BWI.

    Wow…62F is the record.  Lowest record high max of the entire month and only set 2 years ago!  That's a gimmee.  IAD's record is 61F, also set in 2011.  Both of those are probably locks.  DCA is 68F.  That's going to be close.  

  6. Speaking of CAPE and following up about the skew-T discussion, the amount of CAPE can be directly calculated from the skew-T by adding up the area between the parcel trajectory (along a moist adiabat) and the environmental temperature profile. So, if there's a lot of room between the two, you can know the CAPE is high before looking at the calculated parameters directly.

    The "opposite" of CAPE is CIN (convective inhibition) and is also measured in J/kg. CIN occurs when the parcel trajectory will lead it to be colder than the environmental temperature. If the parcel is colder, it's not buoyant in the free atmosphere and needs to be forced to a height in the atmosphere where it is bouyant before it can freely begin to rise. When people speak of a "cap", there means the atmospheric profile has a certain amount of CIN to overcome.

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