I assume you are referring to a rain shadow desert but your question makes little sense as written. A rain shadow desert forms when a mountain range blocks the flow of moisture from reaching the interior of a continent. It forces the ran to fall on the windward side of the mountains and little moisture is able to cross the mountains to the leeward side. See the diagram above.
I don't know, and I don't care. Yes
A scree slope is caused by weather erosion breaking off pieces of rock from the cliff and mountain-side.
Mass wasting is caused when there are loose rocks and soil on a mountain, then somthing moves it. Then it all falls down the mountain causing a landslide. Denver Simmons
No. Cape Town the metropole is mostly flat. The Table Mountain, Constantiaberg and Tygerberg mountain ranges have some suburbs along their foothill edges with great views of the rest of the city. The main business district is in the City Bowl, surrounded by Table Mountain on one side, Signal Hill on another, Table Bay ocean on the third. On the remaining side, the City Bowl opens out on to the Cape Flats where the majority of the suburbs are located. The Cape Flats used to be an ancient sea bed that is now above the sea level. It is mostly sandy dunes, but is definitely not on a slope. The only "slopes" could be the suburbs that are along the mountains. They are by far the most expensive areas because of their great views of the rest of the city. I would estimate that 80% or more of Cape Town would be described as flat, not on a slope. http://mappery.com/maps/Capetown-Tourist-Map.jpg
The four factors of vegetation are climate, soil, topography, and biotic factors. Climate, including temperature and precipitation, influences the types of plants that can thrive in an area. Soil quality and composition affect nutrient availability and plant growth. Topography, such as elevation and slope, can impact sunlight exposure and moisture retention, while biotic factors include interactions with other organisms, such as competition and symbiosis.
The leeward side of a mountain is dry because as air ascends the windward side, it cools and releases moisture as precipitation, leaving less moisture to travel over the mountain to the leeward side, resulting in a rain shadow effect. This creates dry conditions on the leeward slope of the mountain.
A leeward slope is on the opposite side of a mountain, opposite to where the wind is blowing. For example, wind is blowing from north to south to a mountain, and the south side of the mountain would be the leeward slope.
Tokyo is in leeward slope.
THE LEEWARD SIDE IS HOTTER
the windward slope is wetter. the leeward slope is drier. source: geosystems sixth edition by christopherson, page 213 by: josephine
You would typically expect to find the least precipitation on the leeward side, which is the side opposite to the direction of the wind. In this case, it would be the northern slope of the mountain. As the air rises over the mountain, it cools and releases moisture on the windward side, leaving less moisture to fall on the leeward side. This phenomenon is known as the rain shadow effect.
The prevailing winds will force the clouds to climb when they reach the mountain range. As the clouds rise they drop their moisture. So the windward side of the mountain will get rain, and the leeward side of the mountain will be drier.
The leeward side of a dune is shorter and called the slip face. Dunes often serve an important purpose in protecting land from storm waves.
yes
Orographic uplift occurs when an air mass is forced to rise up a mountain slope. As the air rises, it cools adiabatically and condenses to form clouds and precipitation on the windward side of the mountain. On the leeward side, the now drier air descends and warms adiabatically, resulting in a rain shadow effect where little precipitation falls.
You would expect to find the precipitation on the windward slope, which in this case would be the south side of the mountain. As the air rises and cools when it hits the mountain, it reaches its dew point and condenses into precipitation. This leaves the leeward side, or the north side in this scenario, in a rain shadow with less precipitation.
The difference is that windward gets more rain, is wetter, and is the side of the mountain that is closest to the ocean. On the other hand the leeward is the farthest from shore and is drier but still gets rain.