Mid-Term Review Flashcards
earths energy budget
25% reflected by clouds and particules
20% absorbed by particuls In the atmosphere
50% absorbed by earths surface (land and water)
5% reflected by land and sea surface
albedo
the colour of a surface effects how much energy it will absord
-low albedo=dark surfaces absord more energy
-high albedo=light surfaces reflect energy
hydrosphere
total amount of water on a planet
how does the hydrosphere act as a heat sink
Water is a good heat sink and has a high heat capacity and so when the hydrosphere gets warm it holds a lot of heat and creates a heat sink compared to land that has a low heat capacity
radiation
heat transferred to an object without direct contact
conduction
heat being transferred from a object with higher temperature to an object with a lower temperature through direct physical contact
convection
the transfer of thermal energy by vertical movement from one place to another
greenhouse effect
Greenhouse effect is where the sun’s solar energy comes into the Earth’s atmosphere but the Earth’s atmosphere traps some of the gases in to keep the earth warm. this causes the troposphere to retain more heat than it would if the gases were not present causing the Earth’s atmosphere to act as a heat sink
how are high-pressure systems formed
-An air mass cools over an ocean or a cold region on land as the air mass cools particles in the air lose kinetic energy in the air becomes denser the air mass contracts pulling down air from the upper troposphere and the added weight of extra air increases the atmospheric pressure -wind results in air moves from an area of high pressure to low pressure
-moves clockwise in the northern hemisphere
how are low-pressure systems formed
-An air mass warms over land or water
-as the air mass warms particles in the air gain kinetic energy and the air becomes less dense expands and Rises
-the warm air cools as it rises producing clouds and precipitation
-wind moves counterclockwise in the northern hemisphere
artic air mass
winter= bitter col, dry
summer= cold, dry
continental polar
winter= very cold, dry
summer= cool, dry
continental tropical
winter= warm, dry
summer= hot, dry
maritime polar
winter= cold, humid
summer= cool, humid
maritime tropical
winter= warm, humid
summer= hot, humid