FLURRIES OR FEET? An Analysis of QPF Errors in an Eastern North Carolina Snowstorm December 2-4, 2000 Jason Caldwell South Carolina State Climate Office.
Topic 0.2 – Observations and Forecasts of Wind Distribution Kevin CHEUNG (USA) Akhilesh GUPTA (India) Bruce HARPER (Australia) Jeff KEPERT (Australia)
Chapter 12 Tropical Storms and Hurricanes. Extremely strong tropical storms go by a number of different names, depending on where they occur. Over the.
How do the clouds form?. Water Vapor Basics (names of different phase changes, latent heat) Humidity indices (there are 6 total). Saturation vapor pressure.
The Thermostat Hypothesis Jesse Vannatta Major: Atmospheric Science.
PRESSURE SYSTEMS, AIR MASSES & FRONTS Basic Climatology Oklahoma Climatological Survey Funding provided by NOAA Sectoral Applications Research Project.
Cumulus Forced; pushed upward by external forces, i.e. lifting by surface convergence, topography etc. Active; growing upward from self-forcing, i.e. buoyancy,
NATS 101 Lecture 19 Monsoons. Supplemental References for Today’s Lecture Aguado, E. and J. E. Burt, 2001: Understanding Weather & Climate, 2 nd Ed. 505.
The Inland Extent of Lake Effect Snow (LES) Bands Joseph P. Villani NOAA/NWS Albany, NY Michael L. Jurewicz, Sr. NOAA/NWS Binghamton, NY Jason Krekeler.
Atmospheric Controls on North African Dust Emission Richard Washington Sebastian Engelstaedter Martin Todd, Gil Lizcano Fiona Mitchell Yoram Kaufman, Ilan.
Chapter 10: Middle Latitude Cyclones Chapter 10: Mid-latitude Cyclones Most active weather is associated with a cyclone (i.e. low pressure system) Here.
Ocean Gyres - combine knowledge of global winds and Ekman flow - surface transport can be determined from wind direction/velocity - surface transport alters.