An East Coast Winter Storm Precipitation Climatology

Slides:



Advertisements
Similar presentations
Assignment Work: Answer Q 1abc 2ab on pg 98
Advertisements

Chapter 10. Atmosphere Ocean Interactions Global Winds and Surface Ocean Currents Ocean surface dragged by wind, basins react to high pressure circulation.
AGENZIA REGIONALE PER LA PROTEZIONE DELLAMBIENTE DELLA SARDEGNA ARPAS Andrea Motroni Climate, climate change and desertification.
NOAAs National Weather Service Winter Season Outlook 2012 NCEMA Fall Conference Nick Petro, WCM NWS Raleigh, NC Tony Sturey, WCM NWS Greer, SC.
Plant Sector Workshop March 21, MIT – Progress on the Science of Weather and Climate ExtremesMarch 29, 2012 Motivation –Billion-dollar Disasters.
Climate Recap and Seasonal Outlook Dr. John Abatzoglou Assistant Prof, Department of Geography University of Idaho Many Thanks to Eric.
Climatology Lecture 8 Richard Washington Variability of the General Circulation.
Data and Methodology Snowfall totals were derived from the Midwest Regional Climate Center (MRCC) for individual National Weather Service (NWS) Cooperative.
Climate Variability and Irrigation Water Use Joel O. Paz Extension Agrometeorologist Biological and Agricultural Engineering Department The University.
Class #7: Thursday, July 15 Global wind systems Chapter 10 1Class #7, Thursday, July 15, 2010.
UCSB Climate Research Meeting Dept. of Geography ICESS- UCSB October 16, 2009 Earth Space Research Group Climate Variations and Impacts: Monthly Discussion.
 Bodies of air that bring distinctive weather features to the country.  A mass of air in air that is very uniform in temperature, pressure, and humidity.
Long Term Temperature Variability of Santa Barbara Coutny By Courtney Keeney and Leila M.V. Carvalho.
Northeast Regional Climate Center Dr. Art DeGaetano, Professor Department of EAS Director of the NOAA Northeast Climate Center, Cornell.
1 Maryland: Observed and Model Simulated Climate Change. Temperature, Precipitation & Theirs Variability Dr. Konstantin Vinnikov, Acting State Climatologist.
Weather is a description of what the atmosphere is like at a particular time and place. The weather can change from day to day, hour to hour, and from.
North American snowfall variation from a unique gridded data set Daria Kluver Department of Geography University of Delaware.
Synoptic Categorization and climate variability analysis of historical flood- inducing storms in the Northeast Johnathan Kirk Northeast Regional Climate.
Climate Impacts Discussion: What economic impacts does ENSO have? What can we say about ENSO and global climate change? Are there other phenomena similar.
1 Trade Winds in Equatorial Pacific. 2 ITCZ Location July January ITCZ.
Impacts of Climate Change on Physical Systems PPT
The Role of Coupled Jet Streaks in a Midwestern Heavy Snow Event Chad M. Gravelle 1,3, Scott M. Rochette 1, and Thomas A. Niziol 2 1 Department of the.
Outline Background, climatology & variability Role of snow in the global climate system Indicators of climate change Future projections & implications.
MARYLAND’S CLIMATE: VARIABILITY AND CHANGE Dr. Konstantin Vinnikov, Acting State Climatologist for Maryland University of Maryland at College Park, MD.
Evaluating Potential Impact of Significant East Coast Winter S torms by Analysis of Upper and Low-Level Wind Anomalies Neil A. Stuart NOAA/NWS Albany,
Summer 2010 Forecast. Outline Review seasonal predictors Focus on two predictors: ENSO Soil moisture Summer forecast Look back at winter forecast Questions.
An Overview of California Climate Michael Anderson, State Climatologist.
Question and Answer Session Related to the Weather photo: D. Martin Douglas K. Miller Professor and Chair Atmospheric Sciences Department UNC Asheville.
National Climatic Data Center NCDC "State of the climate" search/2008/ann/bams/.pdf and.ppt.
By: Stephanie Paolone and Ben Clarke. small temperature range Bodies of water in the north and south have a warming affect on the Ontario Region ex. Great.
Climate Literacy Session: Climate, Climatology of California Elissa Lynn August 5, 2015.
Verification of the Cooperative Institute for Precipitation Systems‘ Analog Guidance Probabilistic Products Chad M. Gravelle and Dr. Charles E. Graves.
TRENDS IN U.S. EXTREME SNOWFALL SEASONS SINCE 1900 Kenneth E. Kunkel NOAA Cooperative Institute for Climate and Satellites - NC David R. Easterling National.
Precipitation Intensity Climate Impacts Group & Department of Atmospheric Sciences University of Washington Eric Salathé.
An investigation of slow-moving East Coast Winter Storms during the past 55 years Jase Bernhardt Northeast Regional Climate Center Cornell University.
El Nino Teleconnections Philip Kreycik EPS 131 4/30/04.
“Effects of Pacific Sea Surface Temperature (SST) Anomalies on the Climate of Southern South Carolina and Northern Coastal Georgia ” Whitney Albright Joseph.
July 25, 2001 presents “Past, Present, and Future” Ed Kieser.
Air Masses. Differences in air pressure are caused by unequal heating of Earth’s surface – creates wind patterns – Deflects in a curved path because of.
AOS 101 Weather and Climate Lisha M. Roubert University of Wisconsin-Madison Department of Atmospheric & Oceanic Sciences.
C20C Workshop, ICTP Trieste 2004 The impact of stratospheric ozone depletion and CO 2 on tropical cyclone behaviour in the Australian region Syktus J.
2015. equator Normally, trade winds converge at the equator and push warm water westward. In the eastern Pacific, cold water rises to the surface - upwelling.
EARTH’S CLIMATE PAST and FUTURE SECOND EDITION CHAPTER 17 Climatic Changes Since the 1800s WILLIAM F. RUDDIMAN © 2008 W. H. Freeman and Company.
El Nino 101 and Impacts from Recent El Nino Events Chip Konrad Director of the NOAA Southeast Regional Climate Center University of North Carolina at Chapel.
Climate extremes and changes in precipitation and wind patterns ( ) in the vicinities of Montevideo, Uruguay V Pshennikov, M Bidegain, F Blixen,
Local Weather Patterns. Weather Patterns Weather changes from day to day and from season to season. These changes typically happen in the same way, following.
Science 10 Mr. Jean May 7 th, The plan: Video clip of the day Predicting the perfect snow day –Types of storms –Timing –Public Opinion Powerful.
Climatological Aspects of Freezing Rain in the Eastern U.S. Christopher M. Castellano, Lance F. Bosart, and Daniel Keyser Department of Atmospheric and.
Climatology of the Río de la Plata Basin: short and long term variability Mario Bidegain Facultad de Ciencias Universidad de la Republica Uruguay Workshop.
Wind The movement of air.. What causes wind? Caused by: –Heat flow (difference in temperatures) –Pressure differences Cooler air is more dense than warm.
Factors That Affect Climate. Identify five factors that affect climate and explain how each affects climate.
An East Coast Winter Storm Precipitation Climatology
El Niño–Southern Oscillation (ENSO): What is it?
Climate Change Highlands, NC
UMass Lowell Atmospheric Science Program
Examining Major El Nino Events: Impacts on Precipitation and Flood Potential in the Northeast United States.
Moving from Empirical Estimation of Humidity to Observation: A Spatial and Temporal Evaluation of MTCLIM Assumptions Using Regional Networks Ruben Behnke.
El Nino Southern Oscillation
José J. Hernández Ayala Department of Geography University of Florida
The November 26, 2014 banded snowfall case in southern NY
Factors Affecting Climate Gr. 9 Geography
Ed Kieser presents Weather Outlook The 2004 Season March 9, 2004.
What is Weather?
Ch Climate Climatology – the study of Earth’s climate and the factors that affect past, present, and future climatic changes. Climate is the long-term.
Predictive Modeling of Temperature and Precipitation Over Arizona
EQ: What is the impact of climate on Georgia’s growth and development?
Monitoring the Weather
Natural Climate Variability
Northeast snowstorm of 8—10 February 2015
Winter/Spring Outlook:
Presentation transcript:

An East Coast Winter Storm Precipitation Climatology Nicholas J. Frankoski Dr. Arthur T. DeGaetano Cornell University Department of Earth and Atmospheric Sciences Ithaca, NY

Research Objectives Percentage of Snowfall from East Coast Winter Storms (ECWS) Throughout the Eastern United States Percentage of Precipitation from ECWS Throughout the Eastern United States Percentage of Snowfall and Precipitation from Rapidly Deepening Storms (“Bombs”) Throughout the Eastern United States Analysis of Percentages - Trends, Variations, Relationships to El Niño - Southern Oscillation President’s Day Storm of 2003 (NCDC and NOAA)

Climatology of ECWS An East Coast Winter Storm Climatology (Hirsch, DeGaetano, Colucci)

Cooperative Observer Stations collecting daily snowfall data

Determining ECWS Snowfall and Precipitation: The Decision Process

Precipitation (in) 02 Nov 1970 Precipitation Gradient Line Pressure Gradient Line

Average Annual Percentage of Snowfall from ECWS during 1951-1952 to 2005 - 2006

Average Annual Percentage of Precipitation from ECWS during 1951-1952 to 2005 - 2006

Average Annual Snowfall (cm) from ECWS during 1951-1952 to 2005-2006

Average Annual Precipitation (mm) from ECWS during 1951-1952 to 2005-2006

Average Percentage of November Snowfall from ECWS during 1951-1952 to 2005-2006

Average Percentage of November Precipitation from ECWS during 1951-1952 to 2005-2006

Analysis by Region: Based on Average Annual % of ECWS Snowfall Northern New England Appalachians Transition Zone Urban Corridor Southeast Local Minimum Deep South Maximum

Northern New England: ECWS Snowfall (cm), % of Snowfall from ECWS, by snow-year

Next Steps… Sensitivity Analysis: How would the ECWS percentages change if any COOP station in the study having precipitation or snowfall during an ECWS event was included in the climatology? How would the ECWS percentages change around the Great Lakes if Lake Effect snow was included in the climatology?