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Weather Study Notes The water cycle recycles the water and replaces the water on Earth. Only freshwater can evaporate. STUDY YOUR VOCAB FLASHCARDS!!!!!! Make sure you not only know the definitions, but also can give examples. Angle of insolation affects temperature, the closer you are to the equator the hotter the temperature is. Air pressure = stacking hands As you go higher in the atmosphere the temperature and air pressure decrease. All life and weather happen in the troposphere layer of the atmosphere. As water vapor rises it CCC…cools, condenses and forms a cloud. Humidity = feeling sticky, frizzy hair, or fogged up glasses Morning Dew = condensation Sidewalk drying (or puddle) = evaporation Cloud formation pictures Types of Clouds and their precipitation Cloud Cirrus ● ● ● ● Precipitation High in the atmosphere Ice crystals Wispy and feather like Cirrus cumulous clouds “snow storms” Snow Stratus Blanket like layers Cumulous Puffy and rise up from a flat bottom Cumulonimbus ● ● ● ● ● ● Long lasting Smaller raindrops Heavy rain last for a short period of time ● ● ● ● ● ● Rain or storms Gray or black Vertical (develop upward) thunderstorms Larger raindrops Hold a lot of water Turbulent (violent) Can reach high altitudes Downpours HAIL Fog ● ● ground level moist air at ground level cools Air Pressure can change due to volume (more area less pressure), elevation (higher less pressure), temperature (warmer temperature give lower air pressure), and humidity (moist sir has less pressure than dry air) Air pressure moves from high pressure to low pressure Convection Cell Picture: HOT AIR RISES AND COLD AIR SINKS Land will cool quicker and water will hold heat longer than land Night = land to sea = land breeze (warm breeze)…mountain Day = sea to land = sea breeze (cool breeze)…valley Coriolis Effect Picture Global Wind Patterns Picture We live in the PREVAILING WESTERLIES; this means our weather moves from WEST to EAST in the United States. High pressure = happy weather and sunshine Low pressure = lousy weather and rain High pressure systems (H) = high pressure in the center, winds blow outward, and winds blow clockwise. Remember your hand activity… Low pressure systems (L) = lower pressure in the center, winds blow toward the center, and winds blow counterclockwise…Remember you hand activity… High and Low Pressure System Pictures Weather Station Models and Cloud Cover Pictures Air masses move west to east or left to right Air masses over water will be moist, air masses over land will be dry Equator = hot Poles = cold Continental = land Maritime = water When warm air masses and cold air masses meet they form storms Cold front = cold air moves in under warm air and pushes the warm air up (remember cold air is the bully because it is heavier), brings brief heavy storms or thunderstorms with strong winds, and after the storm the skies are clear cool and dry. Warm front = warm air moves in over a cold air mass, brings light steady rain or snow that lasts for days with light winds and sometimes fog, and after the storm the weather is warmer and humid. Stationary Front = warm air mass meets a cold air mass and they to do not move each other Electrical charges build up in a cloud = lightening (heats the air causes thunder) Tornados = runaway convection cell = wind funnel with thunderstorms Tornado Alley = Midwest region of the US = most tornados occur Hurricanes have low pressure in the center “eye of the storm is clam Hurricanes form over warm water and bring a lot of rain that can cause flooding Climate is determined by weather data collected every day over a period of time Climate = precipitation + temperature Climates = Biomes Affects of Climate = latitude (the farther away from the equator the colder it is), Water (closer to water gives you sea breezes), and altitude (higher in the atmosphere gives you colder weather) Rain shadow Picture Climate change = global warming = ozone layer = pollution US weather patterns are formed by the Jet Stream = prevailing westerlies El Niño is characterized by unusually warm ocean temperatures in the Equatorial Pacific, as opposed to La Niña, which characterized by unusually cold ocean temperatures in the Equatorial Pacific. El Niño is an oscillation of the ocean-atmosphere system in the tropical Pacific having important consequences for weather around the globe. Among these consequences are increased rainfall across the southern tier of the US and in Peru, which has caused destructive flooding, and drought in the West Pacific, sometimes associated with devastating brush fires in Australia. Observations of conditions in the tropical Pacific are considered essential for the prediction of short term (a few months to 1 year) climate variations.