GEOG 1F91 Lecture Notes - Lecture 4: Jet Stream, Stratopause, Atmosphere Of Earth
Document Summary
Measure of the level of sensible heat (gas, liquid, solid) First thermometer invented by galileo in 1592. Upper boundary and coldest part of the atmosphere (-90. Small changes in solar energy= large changes in temperature. Key variables of temperature: insolation, latitude (tilt, rotation, cloud cover, surface type, proximity to water, elevation, slope and aspect. Thermal properties =temperature difference coast and interior. Coastal temperatures less variable day/night and summer/winter. Earth"s revolution + tilt = annual cycle of net radiation. E. g: areas of perpetual ice and snow are always intensely cold e. g. isotherms make a large n-s shift from january to july over, isotherm patterns are associated with ocean currents. Rockies and andes polar regions continents in the mid-lat. Bubbles of gas in ice e. g. ghg conc. Measure ring width and match patterns in growth. Historic documents are valuable sources of past climate.