Answer:
Adiabatic stability
Explanation:
Adiabatic stability - Adiabatic implies a situation in which the air parcel and the surrounding region do not exchange heat. It will ultimately undergo cooling whenever a parcel of air increases. Latent heat does not release whenever unsaturated air parcel moves in an upward direction.
Cooling will occur quickly as air parcel is unsaturated, the cooling is at a rate of 10 °C / km. This is called the dry adiabatic rate of lapse. Once the parcel of air becomes sufficiently dense it will start sinking.
Answer:
Songs and Quizlets
Explanation:
When I study maps I look up little jingles online, for example I had to memorize as many countries as possible so I looked up “songs to memorize the worlds countries” if I can’t find a song I normally make one up. I also try to make quizlets (online study cards) these are things that norm help me and I hope they help you!
Slitstone
Hope this helped!
Answer: B) The mantle is hotter than the crust.
Explanation: the heat energy is transferred to multiple layers eventually losing it's high temperature in each layer and the crust is the the surface layer and the mantle is closest to the core which is very hot and the heat projected from the mantle has time to lose it's heat when it's heat is transferred through the many layers of the earth. Hope this helped somebody learning geography.
