Heat Transfer

John Dalton

James Dewar

John Edison

James Blake

more warm air from sea

cool air from sea

more cool air from land

warm air from land

warm

hot

cool

normal

absorb more heat

absorb less heat

reflect more heat

transfer less heat

environment

surroundings

trees and forests

glaciers

excess heat loss

excess heat absorption

excess heat loss and absorption

excess heat transfer

water

solids

sand

vacuum

remains same

stops

is reversed

is converted to radiation current

electrical insulator

electrical conductor

thermal conductor

thermal insulator

different sizes of lines on a photograph

different shapes on a photograph

different colors on a photograph

different images on a photograph