The Atlantic and Gulf Coastal Plain physiographic province has which of the following characteristics?   Many fertile swamps and marshes   Low, rolling hills   Folding, uplift, and faulting   Small mountain ranges and flat valleys

Suppose you are visiting the equator. It is noon. The Sun is at its highest point in the sky for the day, which is directly over your head. You call a friend on the phone, and she says it is also noon where she is but the Sun is not directly overhead at that location and time. It is a little lower in the sky for her. Compare the longitude and latitude of your location with the longitude and latitude of your friend's location. Are they alike or different? How do you know?

Provide examples to illustrate the effects of glacier and ice sheet melting on climate globally and regionally. Use words to illustrate any feedback mechanisms between melting ice sheets and the climate.

Use diagrams and word explanations to show how excess heat from the tropics is transferred to higher latitudes (discuss cells and ciruclations) . Additionally, show how the broadening of the Hadley Cell,  caused by rising greenhouse gases, could affect surface climate in subtropical and mid-latitude regions.

Explain why the Earth is in not in radiative equilibrium

Showing the energy flows into and out of Earth’s atmosphere with energy sketches. Clearly label each flow for what it represents, distinguishing between solar and terrestrial energy flows.  Explain the diagrams in more details

44) In periglacial environments, the layer of ground that thaws every summer and freezes every winter is called A) frost layer B) permafrost C) active layer D) discontinuous permafrost

Use the attached piezometer map to make your own, clean version of the map, and indicate the elevation of the water table at all piezometer locations. Draw equipotential lines (lines of equal water table elevation) using regular intervals – creating a contoured map of the water table. Determine the direction of groundwater flow based on the horizontal gradient. Label  the areas of recharge and discharge directly on your map. Flow lines: Draw flow lines on your water table map. The lines should be at right angles to the equipotential lines and extend from the recharge area to the discharge area. Hydraulic Gradient, Specific Discharge (Darcy Flux), Average Linear Velocity:  Using your water table map, estimate an average hydraulic gradient between two locations, call them locations A and B, one at the eastern-most and a second at the western-most extent of your dataset (note the north arrow on the map). Calculate the specific discharge, q, between the two locations. For this calculation…

Calculate all the values of table 1: Q in (L/day) Q out (L/day) Residence time (days) Please show all steps