Areas that receive over 400 cm of rainfall are rain forests. The areas that receive less than 20 cm of rainfall are desert areas.
The usual antonym for receive is give. It is more blessed to give than it is to receive.
John Napier did not receive any at all. He is simply nowadays noted as the creator of logarithms.
Give, receive...
I need to know how do you figure out the percentage if you receive 3500 dollars which is 30 percent of what total?
A windward island refers to an island that is located to the east of prevailing winds. These islands typically receive more rainfall and have lush vegetation compared to leeward islands located to the west. Examples include islands in the eastern Caribbean such as Martinique and Barbados.
The windward side of mountains receives large amounts of rainfall because as the moist air is pushed up the slope, it cools and condenses, leading to precipitation. This process, known as orographic lift, causes the air to release its moisture as rain or snow as it ascends the mountain.
Due to the change in atmospheric conditions a mountain can cause, the windward side of the mountain received the rain while the leeward side of the mountain does not receive the moisture creating a desert landscape. As the moisture rises to overtake the mountain the clouds condense creating rain on the windward side which creates an atmosphere of little to no moisture on the leeward side of the mountain.
Although Kauai is known as the "wetest spot on earth", rainfall amounts vary greatly throughout the Garden Island. The Makai (beach side) areas generally receive far less rainfall than the Mauka (mountain) areas. Of course, annual rainfall varies from year to year as well as from the Windward to Leeward sides. Ranfall ranes from 30 inches to 260 inches.
This is false most of the precipitation from moisture laden winds from the sea does not fall on the leeward side of mountains. Many deserts are located in the interior of continents, far from moisture- laden winds blowing from the ocean.
Areas with dry leeward sides of mountains are called rain shadows. These areas receive significantly less precipitation due to the phenomenon where moist air rises over the windward side of a mountain, cools, condenses, and releases its moisture as precipitation, leaving the leeward side dry. Examples include the Great Basin in the United States and the Atacama Desert in South America.
A mountain range can act as a barrier to air movement, causing one side to receive more rainfall (windward side) and the other side to be drier (leeward side). This creates a rain shadow effect, influencing temperature and precipitation patterns in the region. Additionally, mountains can impact local wind patterns and create microclimates with varying conditions.
The Lesser Antilles are a chain of islands located in the Caribbean Sea, east of Central and South America. The islands are divided into two main groups: the Windward Islands and the Leeward Islands. The Windward Islands are located to the north and east of the Lesser Antilles, and include the islands of Dominica, Martinique, Saint Lucia, Saint Vincent and the Grenadines, and Grenada. These islands are called the Windward Islands because they are located on the windward side of the Lesser Antilles, which means that they are more exposed to the prevailing easterly winds and tend to receive more rainfall as a result. The Leeward Islands are located to the south and west of the Lesser Antilles, and include the islands of Antigua and Barbuda, Montserrat, Guadeloupe, Marie-Galante, Dominica, Saint Martin, and the British and US Virgin Islands. These islands are called the Leeward Islands because they are located on the leeward side of the Lesser Antilles, which means that they are sheltered from the prevailing winds and tend to be drier than the Windward Islands. Both the Windward Islands and the Leeward Islands are home to a diverse range of cultures, languages, and landscapes, and are popular destinations for tourists seeking beautiful beaches, tropical weather, and a rich history and culture.
The regions in the interior of the Deccan Plateau and the Sahyadris receive low rainfall due to the rain shadow effect. This occurs because the Western Ghats block the moisture-laden winds coming from the Arabian Sea, causing precipitation to fall on the windward side (coastal areas) and leaving the leeward side (interior plateau) relatively dry.
Elevation affects climate by influencing temperature and precipitation patterns. Generally, as elevation increases, the temperature decreases, leading to cooler conditions. Higher elevations also tend to receive more precipitation due to orographic lift, where air masses are forced to rise over mountains, leading to increased rainfall or snowfall on the windward side and drier conditions on the leeward side.
The windward coasts of Hawaii, which face the prevailing trade winds, tend to receive the most annual rainfall. Areas on the eastern and northeastern sides of the Hawaiian Islands typically experience higher levels of precipitation due to the moist air being forced upward by the mountains, leading to increased rainfall.
Mountains can create a barrier that influences the movement of air masses, leading to the creation of different climate zones on either side of the mountain range. They can also impact precipitation patterns, causing areas on the windward side to receive more rainfall, while the leeward side experiences a rain shadow effect with drier conditions. Additionally, mountains can affect temperature by causing cooling with elevation gain, leading to variations in temperature gradients across different elevations.