Hurricane Gert 12-17 August 2017 Maxwell E

Total Page:16

File Type:pdf, Size:1020Kb

Hurricane Gert 12-17 August 2017 Maxwell E Hurricane Gert 12-17 August 2017 Maxwell E. Torres Force-13 March 5, 2019 1 1. Synoptic History Late on August 2, the National Hurricane Center (NHC) began tracking a tropical wave that was emerging off the west coast of Africa. Early on August 3, the wave emerged over water. Initially in a favorable environment, the wave coalesced rapidly and began to show signs of sufficient organization to be called a tropical depression. However, this period was short-lived as the wave entered a more hostile environment on August 5, resulting in its structure and convection severely diminishing. After this, the wave began moving westward at around 20kt and became elongated. This motion continued for the next five days. The eventually slowed down and turned towards the northwest and regained its compact, circular structure on August 10. On August 11, the wave passed to the north of the Leeward Islands and Puerto Rico. At this point, the wave’s organization increased, and curved convective bands developed around a center of circulation that was getting better defined. At 0000 UTC on August 12, a surface low had formed within the wave around 275 n mi east of the Turks and Caicos Islands and continued to gain convection over the next twelve hours. At 1800 UTC on August 12, while the low was about 230 n mi northeast of the Turks and Caicos Islands, it became well-defined enough to be declared a tropical depression. Within 6 hours, the depression had strengthened into a tropical storm and was given the name “Gert” around 215 n mi northeast of the southeastern Bahamas. Despite conducive sea surface temperatures (SSTs) and low wind-shear, Gert failed to intensify for the first 18 hours due to relatively dry air in its environment. By 0000 UTC on August 14, Gert had expelled the dry air and begun to intensify. This steady intensification would continue for the next 3 days. At 0600 UTC on August 15, Gert became a hurricane while located roughly 380 n mi west of Bermuda. Shortly after becoming a hurricane, Gert began to accelerate towards the northeast, having come under the influence of a mid-latitude shortwave trough that was moving off the United States’ east coast. At 1800 UTC on August 16, Gert reached its peak intensity estimated at 100kt while located 385 n mi southeast of Halifax, at which time, its eye measured 10 n mi in diameter. Within 6 hours of reaching its peak, Gert began to move over much cooler SSTs an encountered over 30kt of vertical wind shear. As a result, Gert’s convective cloud pattern quickly eroded, and it weakened to a tropical storm by 1200 UTC on August 17. 6 hours after weakening to a tropical storm, Gert fully transitioned into an extratropical cyclone 290 n mi southeast of St. John’s. the extratropical remnants of Gert moved steadily in a northeasterly direction for over a day while continuing to weaken. At 0000 UTC on August 19, the system dissipated completely over cold waters in the far northern Atlantic Ocean. 2 Meteorological Statistics Wind and Pressure Gert’s estimated peak wind speed of 100kt is based on several satellite estimates from the NHC’s Tropical Analysis and Forecast Branch (TAFB), the Advanced Microwave Sounding Unit (AMSU) and Advanced Dvorak Technique estimate. These estimates give a range of 90kt to 115kt, most of which are near, at, or above 100kt. Averaging these values gives a value between 100kt and 105kt. Because of its small eye, it was likely at the lower end of the averaged range. Thus, a value of 100kt has assigned as Gert’s peak intensity. The estimated minimum central pressure of 960mb is based on the NHC’s wind- pressure relationship estimate of 962mb accounting for the slight increase of wind speed from their 95kt value. Casualty and damage Statistics There are no reports of damage associated with Gert. However, two drownings in high surf are believed to be associated with Gert. Best Track Below is the best track chart for Hurricane Gert Date Time (UTC) Lat. Lon. Wind (kt) Pressure SSHWS (mb) 8/12 0000 22.4 66.8 25 1013 LOW 8/12 0600 22.7 67.8 25 1013 LOW 8/12 1200 23.2 68.7 25 1013 LOW 8/12 1800 24.0 69.4 30 1013 TD 8/13 0000 24.9 70.0 35 1012 TS 8/13 0600 25.8 70.6 35 1012 TS 8/13 1200 26.8 71.2 35 1012 TS 8/13 1800 27.7 71.6 35 1012 TS 8/14 0000 28.5 71.9 40 1009 TS 8/14 0600 29.2 72.1 45 1006 TS 8/14 1200 29.7 72.2 50 1002 TS 8/14 1800 30.2 72.3 55 996 TS 8/15 0000 30.8 72.3 60 992 TS 8/15 0600 31.5 72.3 65 986 1 8/15 1200 32.3 72.1 70 982 1 8/15 1800 33.2 71.8 70 980 1 3 8/16 0000 34.2 71.0 70 976 1 8/16 0600 35.4 69.5 80 973 1 8/16 1200 36.8 67.1 90 969 2 8/16 1800 38.2 64.1 100 960 3 8/17 0000 39.4 60.4 90 964 2 8/17 0600 40.7 56.2 80 968 1 8/17 1200 42.2 52.0 60 981 TS 8/17 1800 44.0 48.0 50 988 EXTRATROP. 8/18 0000 45.9 44.3 40 991 EXTRATROP. 8/18 0600 47.7 40.5 35 994 EXTRATROP. 8/18 1200 48.8 37.8 35 996 EXTRATROP. 8/18 1800 50.5 36.5 35 998 EXTRATROP. 8/19 0000 DISSIPATED 4 Below is the best-track map for Hurricane Gert 5 Forecasting and Warning Critique The precursor to Gert was never well forecast, having fluctuated between low, medium, and high chances of formation twice on the 48-hour and 5-day outlooks from the NHC before it finally formed. With the 48-hour outlook reaching a medium chance (40-60%) twice and the 5-day outlook reaching a high chance (>60%) twice prior to formation. After formation, Gert was forecast much better, with the only critique being the fact that it became a hurricane around a day before it was originally forecast to. Because it never got close to land as a tropical cyclone and was never expected to, no tropical cyclone watches or warnings were issued in association with Gert. 6 Cyclone Destruction Potential Scale since January of 2017, Force Thirteen has rated storms used the Cyclone Destruction Potential Scale (CDPS), a scale developed by member Devon Williams with the intention of determining how destructive a storm will be using multiple factors and presenting it to the public in an easily understandable way. The result is a ten-tiered scale that encompasses tropical storms as well as hurricanes. Hurricane Gert is estimated to have reached stage 5 on the old CDPS used from January of 2017 to December of 2018. A stage 5 is described as a powerful storm that will cause devastating damage. Because Gert never impacted land and rainfall estimates weren’t available at the time, no estimate has been or will be made using the new CDPS that was first used in January of 2019. 7 Other Data The following are sets of miscellaneous data from Gert throughout its life time. 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 .
Recommended publications
  • HURRICANE KENNETH (EP132017) 18–23 August 2017
    NATIONAL HURRICANE CENTER TROPICAL CYCLONE REPORT HURRICANE KENNETH (EP132017) 18–23 August 2017 Robbie Berg National Hurricane Center 26 January 2018 NASA-NOAA SUOMI NPP ENHANCED INFRARED SATELLITE IMAGE OF HURRICANE KENNETH AT 1034 UTC 21 AUGUST 2017 WHILE AT PEAK INTENSITY Kenneth was a category 4 hurricane (on the Saffir-Simpson Hurricane Wind Scale) over the eastern North Pacific Ocean that did not affect land. Hurricane Kenneth 2 Hurricane Kenneth 18–23 AUGUST 2017 SYNOPTIC HISTORY Kenneth formed from the interaction of two tropical waves which moved off the west coast of Africa on 29 July and 2 August. The first wave moved across the Atlantic Ocean and northern South America at low latitudes and reached the eastern North Pacific Ocean on 8 August. At that point, the wave became more convectively active, but it moved only slowly westward for the next week due to its position south of Hurricane Franklin over the Bay of Campeche. In the meantime, the second tropical wave spawned Hurricane Gert over the western Atlantic, with the southern portion of the wave reaching the eastern North Pacific waters on 12 August. With the subtropical ridge rebuilding over the Gulf of Mexico, the second wave moved at a faster speed toward the west and reached the first tropical wave on 16 August (Fig. 1). The interaction of the two waves caused the development of a low by 1200 UTC 17 August about 530 n mi southwest of Manzanillo, Mexico. Convective banding became more organized and persistent through the day, and the low was designated as a tropical depression by 0600 UTC 18 August about 585 n mi south- southwest of the southern tip of the Baja California peninsula.
    [Show full text]
  • Baseline Assessment Study on Wastewater Management Belize
    Caribbean Regional Fund for Wastewater Management Baseline Assessment Study on Wastewater Management Belize December 2013 Revised January 2015 Baseline Assessment Study for the GEF CReW Project: Belize December 2013 Prepared by Dr. Homero Silva Revised January 2015 CONTENTS List of Acronyms....................................................................................................................................................iii 1. Introduction ........................................................................................................................................................ 1 2. The National Context ....................................................................................................................................... 3 Description of the Country .................................................................................................................. 4 Geographic Characteristics ................................................................................................................. 6 Economy by Sectors ............................................................................................................................ 9 The Environment .............................................................................................................................. 13 Land Use, Land Use Changes and Forestry (LULUCF) ....................................................................... 20 Disasters ..........................................................................................................................................
    [Show full text]
  • Mariner's Guide for Hurricane Awareness
    Mariner’s Guide For Hurricane Awareness In The North Atlantic Basin Eric J. Holweg [email protected] Meteorologist Tropical Analysis and Forecast Branch Tropical Prediction Center National Weather Service National Oceanic and Atmospheric Administration August 2000 Internet Sites with Weather and Communications Information Of Interest To The Mariner NOAA home page: http://www.noaa.gov NWS home page: http://www.nws.noaa.gov NWS marine dissemination page: http://www.nws.noaa.gov/om/marine/home.htm NWS marine text products: http://www.nws.noaa.gov/om/marine/forecast.htm NWS radio facsmile/marine charts: http://weather.noaa.gov/fax/marine.shtml NWS publications: http://www.nws.noaa.gov/om/nwspub.htm NOAA Data Buoy Center: http://www.ndbc.noaa.gov NOAA Weather Radio: http://www.nws.noaa.gov/nwr National Ocean Service (NOS): http://co-ops.nos.noaa.gov/ NOS Tide data: http://tidesonline.nos.noaa.gov/ USCG Navigation Center: http://www.navcen.uscg.mil Tropical Prediction Center: http://www.nhc.noaa.gov/ High Seas Forecasts and Charts: http://www.nhc.noaa.gov/forecast.html Marine Prediction Center: http://www.mpc.ncep.noaa.gov SST & Gulfstream: http://www4.nlmoc.navy.mil/data/oceans/gulfstream.html Hurricane Preparedness & Tracks: http://www.fema.gov/fema/trop.htm Time Zone Conversions: http://tycho.usno.navy.mil/zones.html Table of Contents Introduction and Purpose ................................................................................................................... 1 Disclaimer ...........................................................................................................................................
    [Show full text]
  • MASARYK UNIVERSITY BRNO Diploma Thesis
    MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION DEPARTMENT OF ENGLISH LANGUAGE AND LITERATURE Presentation Sentences in Wikipedia: FSP Analysis Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský Declaration I declare that I have worked on this thesis independently, using only the primary and secondary sources listed in the bibliography. I agree with the placing of this thesis in the library of the Faculty of Education at the Masaryk University and with the access for academic purposes. Brno, 30th March 2018 …………………………………………. Bc. Lukáš Opavský Acknowledgements I would like to thank my supervisor, doc. Mgr. Martin Adam, Ph.D. for his kind help and constant guidance throughout my work. Bc. Lukáš Opavský OPAVSKÝ, Lukáš. Presentation Sentences in Wikipedia: FSP Analysis; Diploma Thesis. Brno: Masaryk University, Faculty of Education, English Language and Literature Department, 2018. XX p. Supervisor: doc. Mgr. Martin Adam, Ph.D. Annotation The purpose of this thesis is an analysis of a corpus comprising of opening sentences of articles collected from the online encyclopaedia Wikipedia. Four different quality categories from Wikipedia were chosen, from the total amount of eight, to ensure gathering of a representative sample, for each category there are fifty sentences, the total amount of the sentences altogether is, therefore, two hundred. The sentences will be analysed according to the Firabsian theory of functional sentence perspective in order to discriminate differences both between the quality categories and also within the categories.
    [Show full text]
  • Preparedness and Mitigation in the Americas
    PREPAREDNESS AND MITIGATION IN THE AMERICAS Issue No. 79 News and Information for the International Disaster Community January 2000 Inappropriate Relief Donations: What is the Problem? f recent disasters worldwide are any indication, Unsolicited clothing, canned foods and, to a lesser the donation of inappropriate supplies remains extent, pharmaceuticals and medical supplies, I a serious problem for the affected countries. continue to clog the overburdened distribution networks during the immediate aftermath of highly-publicized tragedies. This issue per- sists in spite of health guidelines issued by the World Health Organization, a regional policy adopted by the Ministries of Health of Latin America and the Caribbean, and the educational lobbying efforts of a consortium of primarily European NGOs w w w. wemos.nl). I N S I D E Now the Harvard School of Public Health has partially addressed the issue in a com- prehensive study of U.S. pharmaceutical News from d o n a t i o n s (w w w. h s p h . h a r v a r d . e d u / f a c u l t y / PAHO/WHO r e i c h / d o n a t i o n s / i n d e x . h t m). Although the 2 study correctly concluded that the "problem A sports complex in Valencia, Venezuela, which served as the main temporary shel- Other ter for the population displaced by the disaster, illustrates what happens when an may be more serious in disaster relief situa- Organizations enormous amount of humanitarian aid arrives suddenly in a country.
    [Show full text]
  • NRL's Satellite Products & Support for JTWC
    NRL’s Satellite Products & Support for JTWC Jeff Hawkins1 Joe Turk, Tom Lee, Charles Sampson, Kim Richardson1 John Kent 2 Organizations: 1Naval Research Laboratory, Monterey, CA 93943 2Science Applications Inc. Corp (SAIC), Monterey, CA 93940 Sponsors: Oceanographer of the Navy Space and Naval Warfare Systems Command - SPAWAR PMW-155 Office of Naval Research Risk-Benefit Assessment of Observing System Decision Alternatives: 18 June 2001 Tropical Cyclone Web Page http://kauai.nrlmry.navy.mil/tc-bin/tc_home Objective: * Demonstrate utility of passive microwave data for tropical cyclone monitoring: - location - structure-organization/intensity * Provide coincident data sets for a given tropical system at one site. - multi-spectral satellite data. - track and forecast information. Approach: * Process global SSM/I, TMI and geostationary imagery (visible/IR) over “systems”. * Map all data sets to common grid and resolution. * Fill in areas outside of passive microwave swath with coincident vis/IR data. * Automate process and distribute via web page. Multi-Sensor Approach * Vital TC features often cloud obscured in Vis/IR imagery. * Passive microwave data enables the analyst to view below most upper-level cloud decks: - Can map important rainband/eyewall features not evident in many vis/IR images. - Readily permits accurate eye/center locations. - Permits mapping exposed low-level centers. - Enables analyst to view structure changes with time. TRMM Microwave Imagery Relocated Tropical Cyclone Position - JTWC Central Dense Overcast Enclosed Eye with Bands Dvorak IR Enhanced GMS-5 Image TMI 85 GHz Image: 2 minutes after GMS-5 Image TRMM data courtesy of NASA/GSFC Scattering • Scattering is caused by large frozen hydrometeors (graupel, hail, snowflakes).
    [Show full text]
  • Bay Eyes Boost from Reaper Wing
    PANAMA CITY SPORTS | B1 SEC TITLE GAME Three weeks aft er an ugly loss at Auburn, No. 6 Georgia gets its biggest do-over Thursday, November 30, 2017 www.newsherald.com @The_News_Herald facebook.com/panamacitynewsherald 75¢ Bay eyes boost from Reaper wing Schools, builders prep By Collin Breaux mission to a base, there’s a for infl ux of airmen, 747-5081 | @PCNHCollinB certain buzz associated with families to Tyndall [email protected] that,” Laidlaw said Wednes- day. “We recognize there’s TYNDALL AIR FORCE going to be a lot of hard work BASE — A new drone wing here in the near future for slated for Tyndall Air Force those of us who are here, as Base is expected to bring well as those of us coming to 24 aircraft, 1,600 airmen — join us very shortly. ... We’re and the need for more local excited about doing it, for housing, classrooms and spe- sure.” cialized training. The wing of 24 MQ-9 Col. Brian Laidlaw, vice Reaper drones, cutting-edge commander of Tyndall’s remotely piloted aircraft 325th Fighter Wing, said the (RPA), is expected to arrive 325th Vice Commander base is enthusiastic about at Tyndall by 2022, bringing Col. Brian Laidlaw speaks Tuesday’s announcement about 1,600 airmen to Bay Maj. Bishane, a 432nd Aircraft Maintenance Squadron MQ-9 Reaper Wednesday about the new that a new MQ-9 Reaper County by 2020. pilot, controls an aircraft from Creech Air Force Base, Nev. Remotely MQ-9 Reaper wing anticipated wing likely will be coming to “That includes an piloted aircraft pilots work closely with intelligence offi cers, sensor at Tyndall Air Force Base.
    [Show full text]
  • Regional Association IV (North and Central America and the Caribbean) Hurricane Operational Plan
    W O R L D M E T E O R O L O G I C A L O R G A N I Z A T I O N T E C H N I C A L D O C U M E N T WMO-TD No. 494 TROPICAL CYCLONE PROGRAMME Report No. TCP-30 Regional Association IV (North and Central America and the Caribbean) Hurricane Operational Plan 2001 Edition SECRETARIAT OF THE WORLD METEOROLOGICAL ORGANIZATION - GENEVA SWITZERLAND ©World Meteorological Organization 2001 N O T E The designations employed and the presentation of material in this document do not imply the expression of any opinion whatsoever on the part of the Secretariat of the World Meteorological Organization concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. (iv) C O N T E N T S Page Introduction ...............................................................................................................................vii Resolution 14 (IX-RA IV) - RA IV Hurricane Operational Plan .................................................viii CHAPTER 1 - GENERAL 1.1 Introduction .....................................................................................................1-1 1.2 Terminology used in RA IV ..............................................................................1-1 1.2.1 Standard terminology in RA IV .........................................................................1-1 1.2.2 Meaning of other terms used .............................................................................1-3 1.2.3 Equivalent terms ...............................................................................................1-4
    [Show full text]
  • Downloaded 09/30/21 03:20 AM UTC 2292 MONTHLY WEATHER REVIEW VOLUME 130
    SEPTEMBER 2002 BLACK ET AL. 2291 Eastern Paci®c Hurricanes Jimena of 1991 and Olivia of 1994: The Effect of Vertical Shear on Structure and Intensity M. L. BLACK,J.F.GAMACHE,F.D.MARKS JR., C. E. SAMSURY,* AND H. E. WILLOUGHBY NOAA/AOML/Hurricane Research Division, Miami, Florida (Manuscript received 16 May 2001, in ®nal form 21 January 2002) ABSTRACT Shear is a key inhibitor of tropical cyclone intensi®cation. Although its signature is readily recognized in satellite imagery and theoretical or modeling studies provide some insight, detailed observations have been limited. Airborne radar and in situ observations in Hurricanes Jimena of 1991 and Olivia of 1994 are a step toward better understanding. Each storm was observed on two consecutive days. Initially, both had small eyes, 16±18-km radius, and maximum winds of ;57 m s21 over sea surface temperatures (SST) .288C in easterly environmental shear. Jimena maintained constant intensity or weakened gradually for 2 days in 13±20 m s 21 easterly shear. Olivia intensi®ed in8ms21 shear on the ®rst day. Overnight, the shear diminished to reverse and became westerly. On the second day, Olivia weakened as the shear increased to .15ms21 from the west, the storm moved over cooler SST, and became surrounded by dryer air. As convection weakened and the outer rainbands ceased to be effective barriers, relative ¯ow due to the environmental shear penetrated more deeply into the vortex core. In both storms, shear controlled the convective structure. Convection organized itself into axisymmetric rings as Olivia intensi®ed in weak shear. When both storms encountered stronger shear, radar re¯ectivity and vertical motion had strong wavenumber-1 components.
    [Show full text]
  • 2017 North Atlantic Hurricane Season Review
    2017 North Atlantic Hurricane Season Review RMS REPORT Executive Summary THE 2017 NORTH ATLANTIC HURRICANE SEASON will be remembered as one of the most active, damaging, and costliest seasons on record. The 2017 season saw 17 named storms, with 10 of these storms (Franklin through Ophelia) reaching hurricane strength and occurring consecutively within a hyperactive period between August and October. The season will be remembered for its six major hurricanes and specifically for the impacts of three of these storms: Harvey, Irma, and Maria. Hurricane Harvey, the first U.S. major hurricane (Category 3 or greater on the Saffir-Simpson Hurricane Wind Scale) to make landfall since Hurricane Wilma in 2005, made landfall near Rockport, Texas, as a Category 4 storm in late August, thus ending the contiguous U.S. major hurricane landfall drought at 4,323 days. Harvey brought record-breaking rainfall to southeast Texas that resulted in widespread catastrophic and unprecedented inland flooding across the Houston metropolitan area, damaging more than 300,000 structures. The RMS best estimate is that the insured loss from Hurricane Harvey will likely be between US$25 and US$35 billion. This estimate represents the insured loss associated with wind, storm surge, and inland flood damage across Texas and Louisiana. Florida saw its first Category 4 hurricane landfall since 2004 when Hurricane Irma made landfall over the Florida Keys in mid-September. The system later came ashore near Naples, Florida as a Category 3 storm, causing widespread wind damage and flooding across the state. Before impacting Florida, Irma tracked through the Caribbean as a Category 5 hurricane and caused extensive devastation on many islands, ultimately ranking as the strongest hurricane on record to impact the Leeward Islands.
    [Show full text]
  • Upper-Ocean Influences on Hurricane Intensification Modeling Christopher Gerard Desautels
    Upper-Ocean Influences on Hurricane Intensification Modeling by Christopher Gerard DesAutels Submitted to the Department of Earth Atmospheric and Planetary Sciences in partial fulfillment of the requirements for the degree of Professional Masters in Geosystems at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY ay 2000 @ Christopher Gerard IesAutels, MM. All rights reserved. The author hereby grants to MIT permission to reproduce and distribute publicly paper and electronic copies of this thesis document in whole or in part. Author . D ......ent. of arth Atmospheric Department.\ of arth Atmospheric and Planetary Sciences May 5, 2 0001o Certified by 'I~' ' Dr. Kerry Emanuel Professor Thesis Supervisor Accepted by .................................. Dr. Ronald G. Prinn Head, Department of Earth Atmospheric and Planetary Sciences Upper-Ocean Influences on Hurricane Intensification Modeling by Christopher Gerard DesAutels Submitted to the Department of Earth Atmospheric and Planetary Sciences on May 5, 2000, in partial fulfillment of the requirements for the degree of Professional Masters in Geosystems Abstract Hurricane intensification modeling has been a difficult problem for the atmospheric science community. Complex models have been built to simulate the process, but with only a certain amount of success. A model developed by Dr. Kerry Emanuel is much simpler compared to previous studies. The Emanuel model approaches hurricane intensification as an ocean-controlled process where the upper-ocean heat content limits intensification. It is shown that this ocean-based model can produce very accurate results when the true structure of the ocean can be determined. The Ocean Topography Experiment (TOPEX) provides an opportunity for the model to be tested through the use of satellite altimetry.
    [Show full text]
  • Prevailing Windswinds
    PrevailingPrevailing WindsWinds Volume 7,Issue 2 October 2017 The Historic October 3-4, 1987 Snow Event INSIDE THIS By Hayden Frank, Lead Forecaster ISSUE: he first couple days of October usually deliver some of the best weather New England NWS Hazard 2 has to offer. High temperatures average between 65 and 70 degrees and the leaves T may just be starting to show their autumn colors. Accumulating snow during the first half of October is quite rare, but has occurred on a few occasions. Narrowing the goal posts EHWO 2 further, a significant snowstorm in the first week of October is very close to pushing the edge of what is even possible based on climatological records. MIC Musings- 3 The freak destructive snowstorm of October 3-4, 1987 is the earliest accumulating snow on rec- A New Home ord for much of eastern New York, western Massachusetts, and western Connecticut. Not only was this the earliest snowfall on record for much of this region, the amounts were just stagger- ‘17 Southern ing as some locations received 1 to 2 feet of snow. The bulk of the accumulations across west- New England 5 ern Massachusetts and western Connecticut were confined to the higher terrain. However, low- Weather er elevations across eastern New York, particularly just east of the Hudson River, received very Conference significant and historic snowfall. 21” of snow was measured in West Sand Lake, NY at an ele- vation of only 500 feet. Hollings This incredible snowstorm was preceded by 1 to 1.50 inches Undergrad 6 of rain across the region in association with a strong cold Scholars front.
    [Show full text]