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FOSS Weather and Water Glossary FOSS Weather and
FOSS Weather and Water Glossary FOSS Weather and

... the dew point. Dew point: The temperature at which a volume of air is saturated with water vapor; condensation occurs when the temperature drops below the dew point. Downburst: A severe localized downdraft from a thunderstorm, causing damaging winds at or near Earth’s surface. Drought: Less than nor ...
Lecture Packet#1
Lecture Packet#1

... an average rate of 3.5° F per thousand feet (6.5 ° C per kilometer); whereas the stratosphere has either constant or slowly increasing temperature with height. The troposphere is where all of Earth's weather occurs. The boundary that divides the troposphere from the stratosphere is called the "tropo ...
Wind Webquest
Wind Webquest

... 2. “If the number of air molecules above a surface increases, there are more molecules to exert a force on that surface and consequently, the pressure (increases or decreases)? 3. What device is used to measure atmospheric pressure? 4. What unit of measure does aviation and television weather report ...
AOS Mini Vignette
AOS Mini Vignette

... As on Earth, solar heating causes the atmosphere of Mars to expand during the day and contract at night. But there are also seasonal variations. Pressure on Mars averages 6.75 millibars: sealevel pressures on Earth are ...
Wind Web Quest
Wind Web Quest

... 12. Slowly blowing winds will be deflected only a small or large amount. 13. Stronger winds will be deflected a small or large amount. 14. Winds blowing closer to the poles will be deflected more or less than winds at the same speed closer to the equator. 15. What is the influence of the Coriolis F ...
THE WEATHER UNIT PREDICTING WEATHER
THE WEATHER UNIT PREDICTING WEATHER

... The major factor in determining the climate of an area is its latitude. Other factors include how close a place is to land and/or water masses, its altitude (how high it is above sea level), the topography of the land, ocean currents, wind and storm patterns. Latitude is the distance north and south ...
SCI 100 - Meteorology
SCI 100 - Meteorology

... Chapter 8 Questions and Topics to Study (cont’d) What type of air mass would be responsible for the weather conditions listed below? (Write their names and 2-letter designation) (a) hot, muggy summer weather in the Midwest and the East (b) refreshing, cool breezes after a long summer hot spell on t ...
activity - Éclairs de sciences
activity - Éclairs de sciences

... which will be the “0” level of their barometric scale. This line must be drawn quite quickly, while the pressure is the same inside and outside the jar. As the atmospheric pressure changes, the needle will point above or below the line. If the needle points below the line, it indicates low air press ...
El Nino - Cloudfront.net
El Nino - Cloudfront.net

... El Nino Years: The first signs of an El Niño are: • Warm water spreads back from the west Pacific to the east Pacific • Warm air rises near Peru (low pressure), causing rain in the Americas • Decrease in air pressure over central and eastern Pacific Ocean • Winds in the Pacific ocean weaken or stop ...
All About Meteorology - Library Video Company
All About Meteorology - Library Video Company

... One of the questions people frequently ask is:What’s the weather going to be like tomorrow? Knowing what the weather is going to be like an hour, day or week ahead of time impacts the lives of eve ryone around us.Weather affects the safety of ship and airline passengers, the amount of food that farm ...
The Earth`s Atmosphere
The Earth`s Atmosphere

... an average rate of 3.5° F per thousand feet (6.5 ° C per kilometer); whereas the stratosphere has either constant or slowly increasing temperature with height. The troposphere is where all of Earth's weather occurs. The boundary that divides the troposphere from the stratosphere is called the "tropo ...
Overview of the Earth`s Atmosphere
Overview of the Earth`s Atmosphere

... wind chill, frostbite and hypothermia heat exhaustion and heat stroke cold spells, dry spells and heat waves severe thunderstorms and flash floods • The mathematical formula for determining the wind ...
COMMISSION FOR BASIC SYSTEMS OPAG on DPFS
COMMISSION FOR BASIC SYSTEMS OPAG on DPFS

... challenges remain in the development of assimilation techniques that optimize the use of observations in initializing coupled models. The time and space scales associated with seasonal-to-interannual variability (large scale, low frequency) suggest the key information for forecasts will derive mostl ...
Surface Weather Elements
Surface Weather Elements

... dry air masses. It typically lies north-south across the central and southern high Plains states during the spring and early summer, where it separates moist air from the Gulf of Mexico (to the east) and dry desert air from the southwestern states (to the west). ...
Adaptable for Earth Science Classes
Adaptable for Earth Science Classes

... move, but some stationary fronts can wobble back and forth for several hundred miles a day. iv) Cold Front – A boundary between two air masses, one cold and the other warm, moving so that the colder air replaces the warmer air. v) Warm Front – The boundary between two air masses, one cool and the ot ...
Adaptable for Earth Science Classes
Adaptable for Earth Science Classes

... move, but some stationary fronts can wobble back and forth for several hundred miles a day. iv) Cold Front – A boundary between two air masses, one cold and the other warm, moving so that the colder air replaces the warmer air. v) Warm Front – The boundary between two air masses, one cool and the ot ...
Weather Merit Badge
Weather Merit Badge

... converted directly to gas (water vapor) Transpiration – evaporation of water secreted by the leaves of plants - 99% of water taken up by plants is transpired into the atmosphere Condensation – conversion of water vapor into water droplets, seen as clouds, fog, mist, dew, or frost Precipitation – coa ...
full C.V. in  format here.
full C.V. in format here.

... Sutherland, P., W. K. Melville, L. Lenain, N. Statom, 2012, In-situ measurements of the effects of wave breaking on near-surface turbulence. AGU Fall Meeting, San Francisco, USA Sutherland, P., W. K. Melville, L. Lenain, N. Statom, 2012, Measurements of near-surface wave coherent turbulence in the p ...
Adopt-A-Drifter Program Lesson
Adopt-A-Drifter Program Lesson

... years, decades, or longer ...
NOAA explanations of abbreviations etc
NOAA explanations of abbreviations etc

... El Niño - El Niño, a phase of ENSO, is a periodic warming of surface ocean waters in the eastern tropical Pacific along with a shift in convection in the western Pacific further east than the climatological average. These conditions affect weather patterns around the world. El Niño episodes occur ro ...
Proactive Decision Support for Severe Weather - OK-First
Proactive Decision Support for Severe Weather - OK-First

... the spotter a couple of miles south. It was this spotter who gave us first knowledge of the large wall cloud that eventually spawned the tornado that destroyed/severely damaged a dozen homes and apartment buildings. The spotter’s call -- along with a warning from NWS Norman -- caused us to activate ...
Weather - s3.amazonaws.com
Weather - s3.amazonaws.com

... Lightning stroke: flow of current thru air (a poor conductor) from the – to the + Lightning can flow from cloud to ground, cloud to cloud, and from ground to cloud Bright light is caused by glowing air molecules heated by the current Lightning follows the path of least resistance (easiest way to p ...
WPF-Weather101
WPF-Weather101

... Pressure Gradient Force with Coriolis and Friction forces acting on it:" ...
Weather
Weather

... – Solution: additional information, which is statistical and dynamical => use 3D and 4D (VAR) data assimilation, which is used on the basis of incomplete and possibly incorrect observations to analyse the likely current state of the atmosphere and to determine the error in the analysis. – Observatio ...
precipitation rain sleet hail
precipitation rain sleet hail

... Amanda Pierce © 2010 ...
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Marine weather forecasting



Marine weather forecasting is the process by which mariners and meteorological organizations have attempted to forecast future weather conditions over the Earth's oceans. Mariners have had rules of thumb regarding the navigation around tropical cyclones for many years, dividing a storm into halves and sailing through the normally weaker and more navigable half of their circulation. Marine weather forecasts by various weather organizations can be traced back to the sinking of the Royal Charter in 1859 and the RMS Titanic in 1912.The wind is the driving force of weather at sea, as wind generates local wind waves, long ocean swells, and its flow around the subtropical ridge helps maintain warm water currents such as the Gulf Stream. The importance of weather over the ocean during World War II led to delayed or secret weather reports, in order to maintain a competitive advantage. Weather ships were established by various nations during World War II for forecasting purposes, and were maintained through 1985 to help with transoceanic plane navigation.Voluntary observations from ships, weather buoys, weather satellites, and numerical weather prediction have been used to diagnose and help forecast weather over the Earth's ocean areas. Since the 1960s, numerical weather prediction's role over the Earth's seas has taken a greater role in the forecast process. Weather elements such as sea state, surface winds, tide levels, and sea surface temperature are tackled by organizations tasked with forecasting weather over open oceans and seas. Currently, the Japan Meteorological Agency, the United States National Weather Service, and the United Kingdom Met Office create marine weather forecasts for the Northern Hemisphere.
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