Answer to Question 1
the Sun and the earth's interior
Answer to Question 2
Adiabatic temperature changes occur when air expands or contracts and consequently undergoes a pressure change. Adiabatic temperature changes require that no energy exchange takes place with the surrounding environment. Air that is not saturated will cool at 10C/km, known as the dry adiabatic lapse rate, as it rises and expands in the atmosphere. Once the air becomes saturated, however, water vapor in the parcel will begin to condense. This condensation releases latent heat energy into the parcel that becomes sensible heat, partially counteracting the adiabatic cooling that occurs as the parcel continues to expand. For this reason, the wet adiabatic lapse rate is lower than the dry adiabatic lapse rate (about 5C at its lowest).
The absorption of light energy by pigment molecules in the light-harvesting complex, and the path th
Color monitor for a computer system.
Procedures and Diagnostic Tests Related to the Endocrine System
Pi molecular orbital system of PLP-amino acid Schiff base
Wind turbines: the fastest-growing energy sector
Male Reproductive System