The top documents tagged [surface convergence]

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
Documents 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

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Topic 0.2 – Observations and Forecasts of Wind Distribution Kevin CHEUNG (USA) Akhilesh GUPTA (India) Bruce HARPER (Australia) Jeff KEPERT (Australia)
Documents Topic 0.2 – Observations and Forecasts of Wind Distribution Kevin CHEUNG (USA) Akhilesh GUPTA (India) Bruce HARPER (Australia) Jeff KEPERT (Australia)

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Chapter 12 Tropical Storms and Hurricanes. Extremely strong tropical storms go by a number of different names, depending on where they occur. Over the
Documents Chapter 12 Tropical Storms and Hurricanes. Extremely strong tropical storms go by a number of different names, depending on where they occur. Over the

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How do the clouds form?. Water Vapor Basics (names of different phase changes, latent heat) Humidity indices (there are 6 total). Saturation vapor pressure
Documents How do the clouds form?. Water Vapor Basics (names of different phase changes, latent heat) Humidity indices (there are 6 total). Saturation vapor pressure

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The Thermostat Hypothesis Jesse Vannatta Major: Atmospheric Science
Documents The Thermostat Hypothesis Jesse Vannatta Major: Atmospheric Science

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PRESSURE SYSTEMS, AIR MASSES & FRONTS Basic Climatology Oklahoma Climatological Survey Funding provided by NOAA Sectoral Applications Research Project
Documents PRESSURE SYSTEMS, AIR MASSES & FRONTS Basic Climatology Oklahoma Climatological Survey Funding provided by NOAA Sectoral Applications Research Project

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Cumulus Forced; pushed upward by external forces, i.e. lifting by surface convergence, topography etc. Active; growing upward from self-forcing, i.e. buoyancy,
Documents Cumulus Forced; pushed upward by external forces, i.e. lifting by surface convergence, topography etc. Active; growing upward from self-forcing, i.e. buoyancy,

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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
Documents 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

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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
Documents 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

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Atmospheric Controls on North African Dust Emission Richard Washington Sebastian Engelstaedter Martin Todd, Gil Lizcano Fiona Mitchell Yoram Kaufman, Ilan
Documents Atmospheric Controls on North African Dust Emission Richard Washington Sebastian Engelstaedter Martin Todd, Gil Lizcano Fiona Mitchell Yoram Kaufman, Ilan

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Chapter 10: Middle Latitude Cyclones Chapter 10: Mid-latitude Cyclones Most active weather is associated with a cyclone (i.e. low pressure system) Here
Documents Chapter 10: Middle Latitude Cyclones Chapter 10: Mid-latitude Cyclones Most active weather is associated with a cyclone (i.e. low pressure system) Here

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Ocean Gyres - combine knowledge of global winds and Ekman flow - surface transport can be determined from wind direction/velocity - surface transport alters
Documents Ocean Gyres - combine knowledge of global winds and Ekman flow - surface transport can be determined from wind direction/velocity - surface transport alters

216 views