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Northeast snowstorm of 8—10 February 2015 Northeast snowstorm of 8—10 February 2015

Northeast snowstorm of 8—10 February 2015 - PowerPoint Presentation

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Northeast snowstorm of 8—10 February 2015 - PPT Presentation

Rachael Coons 9 December 2016 Motivation Widespread areas of greater than 15cm snowfall in Upstate NY and New England with areas of greater than 30 cm snowfall within this region Third of fourth major snowstorm of the season Boston would go on to break seasonal snowfall record ID: 635890

february 2015 northeast snowfall 2015 february snowfall northeast snowstorm persistent region england upstate snow analysis synoptic moisture convergence boston

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Slide1

Northeast snowstorm of 8—10 February 2015

Rachael Coons

9 December 2016Slide2

Motivation

Widespread areas of greater than 15cm snowfall in Upstate NY and New England with areas of greater than 30 cm snowfall within this region.

Third of fourth major snowstorm of the season. Boston would go on to break seasonal snowfall record.

Impacts enhanced by snow still present from previous storms.

https://cbsboston.files.wordpress.com/2015/02/boston-snow-pile.jpg

http://www.wpc.ncep.noaa.gov/winter_storm_summaries/event_reviews/2015/Northeast_US_WinterStorm_Feb2015.pdfSlide3

Data and Methodology

8—10 February 2015 Northeast Snowstorm

NCEP-NCAR reanalysis

WPC surface analysis

Synoptic analysis of case using maps made in GEMPAKSlide4

Synoptic Overview

Divergence in right entrance region of jet over Northeast and left exit region of jet over Southeast

Warm air advection in Upstate New York and New England

Cold air damming with High Pressure centered over Hudson Bay helping to promote easterly flow onshore in New England promoting development of a coastal front.

Persistent moisture convergence throughout eventSurface temperatures 15o-25o

F inland, around freezing on coast.Slide5

00z 8 February 2015

10z 9 February 2015

18:30z 9 February 2015

http://www2.mmm.ucar.edu/imagearchive/Slide6

Conclusions

Forcing at upper and lower levels to support ascent and persistent precipitation.

High

precipitable

water values and persistent moisture convergence supported large snowfall totals. Local maxima where coastal front developed and in higher terrain in southern Vermont.