Schematic energy balance of ideal surface R N = H S + H L + H G Atm S 547 Lecture 10, Slide 1
Energy balance: Dry desert lakebed Atm S 547 Lecture 10, Slide 2
Surface energy balance: barley field Atm S 547 Lecture 10, Slide 3
Energy budget: Fir canopy Atm S 547 Lecture 10, Slide 4
Atm S 547 Lecture 10, Slide 5
Diurnal cycle of surface radiative flux components Atm S 547 Lecture 10, Slide 6
Diurnal cycle of subsurface temperature Arya Atm S 547 Lecture 10, Slide 7
Annual cycle of subsurface temperature Arya Atm S 547 Lecture 10, Slide 8
Surface material properties Atm S 547 Lecture 10, Slide 9
Idealized temperature wave vs. depth Atm S 547 Lecture 10, Slide 10
Annual observed temperature wave vs. depth Atm S 547 Lecture 10, Slide 11
Recommend
More recommend