unit 4 Flashcards
rocks, atmosphere, currents
Climate
the average course or condition of the weather at a place usually over a period of years as exhibited by temperature, wind velocity, and precipitation
weather
the state of the atmosphere at a place and time as regards heat, dryness, sunshine, wind, rain, etc
Troposphere
lowest layer of the Earths atmosphere, almost all weather occurs here, most mass of the atmosphere is here, density and temp decrease
Stratosphere
2nd layer, temp increases with hight, ozone layer is here
Mesosphere
3rd layer, thick gases, slow meteors, middle atmosphere, temp decreases up
Thermosphere
4th layer thin gases, temp increases up, absorbs ultraviolet and x-ray radiation,
exosphere
furthest out, atoms and molecules escape into space, satellites orbit the earth
Albedo
the fraction of light that a surface reflects. If it is all reflected, the albedo is equal to 1. A global increase in albedo would reflect ore solar radiation back into space, potentially stabilizing or even cooling the Earth’s temperature.
Atmospheric convection current
global patterns of air movement that are initiated by the unequal heating of Earth
Insolation
The amount of incoming solar energy that makes contact with the surface of the Earth. Regions of the Earth near the Equator come into closer contact with the Sun, meaning they receive higher insolation than regions closer to the poles
Convection cells
an zone where hot fluid rises while cold fluid sinks, resulting in a circulation of fluid. There are three main ones in each hemisphere rotating in opposite directions; Polar, Ferrell, Hadley.
Coriolis effect
the apparent deflection of moving objects caused by the rotation of the Earth. It causes objects to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere
Rain shadow
an area of significantly reduced rainfall behind a mountainous region on the side facing away from prevailing winds
Gyre
Large circular ocean currents formed by global wind patterns, gravity, temperatures, and forces created by Earths rotation, clockwise in Northern Hemisphere, counterclockwise in Southern Hemisphere
Upwelling
A process in which deep, cold water rises toward the surface bringing many nutrients to the top. Caused by wind blowing across the ocean surface to replace the water that was pushed away
Thermohaline circulation
Deep ocean currents driven by differences in the water’s density. Large water conveyer belt that travels water all across the world.
ENSO
El Niño and La Niña are the war and cool phases of a natural climate pattern across the tropical Pacific. The pattern shifts back and forth irregularly every two to seven years, bringing predictable changed in ocean temperature and disrupting the normal wind and rainfall patterns across the tropics.
La Niña
Cooling of the ocean surface. The normal easterly winds along the equator become even stronger Causes drier-than-average winter in the southern part of the country.
El Niño
Warming of the ocean surface in the central and eastern tropical Pacific ocean. The low level surface winds weaken or start blowing the opposite direction