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The elevation difference between two side-by-side contour lines is known as the contour interval. It represents the vertical distance in elevation between each contour line on a topographic map.
The strongest part of a hurricane is the eyewall. The strongest winds are usually on the right-hand side of the eyewall relative to the storm's motion.
When an air mass is forced to rise above a topographic barrier, such as a mountain range, it undergoes adiabatic cooling. As the air ascends, it expands and cools, leading to the condensation of moisture and the formation of clouds, often resulting in precipitation on the windward side of the barrier. This phenomenon is known as orographic lifting. Conversely, the leeward side typically experiences drier conditions, often referred to as a rain shadow effect.
On a topographic map, you can identify a hill by examining the contour lines. Contour lines that form closed loops are an indication of a hill or a mountain. The closer the contour lines are together, the steeper the slope of the hill.
Its the left side of the brain that is injured As the right side of your brain controls the left side of your body as the left does your right.
The terrain is the steepest when it's on the left side of the map.
The "neat" line.
The difference in elevation between two side-by-side contour lines on a topographic map is called the contour interval. It represents the vertical distance between each contour line and helps depict the steepness of the terrain.
grill
the roc part is the music that he listen to the royal part is his soft side
I have taken a side. J'ai pris un côté.
The far side of the Moon.
Either side
car trunk compartment
middle, top, bottom and side
The right side of your head means that you are already taken
Orographic fog is produced when moist air is lifted over a topographic barrier, such as a mountain range. As the air rises, it cools and condenses to form fog on the windward side of the barrier.