Tropical rain belt


and the tropical climate dominate the tropical rain belt, which oscillates from the northern to the southern tropics over the course of the year, roughly following the solar equator. The tropical rain belt is an area of active rain that is positioned mostly around the tropics.
According to the website Journey North, the reason the rain belt is situated near the tropics can be attributed to the fact that most of the sun's radiation is directed toward the equator, which is located in the middle of the tropics. This solar radiation generates large amounts of heat near the equator providing tropical regions with higher temperatures than most other regions on Earth.
With all this solar radiation, the air around the tropics begins to warm up. Because hot air is less dense than cold air, the hot air rises into the upper levels of the atmosphere and as a result, cold air filters down into the lower levels of the atmosphere. The dynamics that provide the tropics with the rain belt are founded on the principle that warmer air is able to retain more moisture than colder air.
When the colder air replaces the warmer air in the lower atmosphere, the abundant moisture from the tropics loses the ability to be stored in the atmosphere. As a result, the excess moisture that cannot be held by the colder air is then turned into thunderstorms and rain showers. These thunderstorms and rain showers are usually located along the equator, but they will extend out to the Tropic of Cancer, which is the 23.5 north latitude, as well as the Tropic of Capricorn, which is the 23.5 south latitude. It is largely a manifestation of the ITCZ.
The tropical rain belt lies in the southern hemisphere of the Indian ocean and western Pacific ocean roughly from October to March, and during this time the northern tropics experience a dry season in which precipitation is very rare, and days are typically hot and sunny throughout. From April to September, the rain belt lies in the northern hemisphere, and a wet season occurs there, while the southern tropics experience their dry season.
The rain belt reaches roughly as far north as the Tropic of Cancer and as far south as the Tropic of Capricorn in the western Pacific Ocean. Its variation in the Western Hemisphere is minimal, roughly between the equator and the 15th parallel north latitude. Near these latitudes, there is one wet season and one dry season annually. On the equator, there are two wet and two dry seasons as the rain belt passes over twice a year, one moving north and one moving south. Between the tropics and the equator, locations may experience both a short wet and a long wet season. Local geography may substantially modify these climate patterns.

Northward movement and the effects

As the earth warms, the rain belt is projected to move north of the current position. Recent climate change can be attributed to rising carbon dioxide concentrations in the atmosphere; caused by the burning of fossil fuels. The correlation between the concentration of carbon dioxide in the atmosphere and average global temperature is undeniably direct, meaning that as more carbon dioxide is released into the atmosphere, the temperature of the earth is expected to rise as well. Even though the earth is warming as a whole entity, the Northern Hemisphere is warming faster than the Southern because of melting Arctic sea ice.
As the Northern Hemisphere warms, a temperature gradient is established between the Northern and Southern hemispheres. The warmer temperatures in the Northern parts of the tropics foster an environment more conducive to the development of moisture. The additional moisture is met with a low-level atmosphere that is cooler because the warm air has risen to the higher levels of the atmosphere.
This scenario leads to increased precipitation and is a fundament behind the idea that the rain belt is moving north. The contrast in temperature is only a part of the entire process that is driving the tropical rain belt northward. Another factor that influences the tropical rain belt is ocean circulation. Ocean Overturning Circulation is a process that involves ocean circulation between the Antarctic and Arctic regions.
Dargan Frierson explains that in this process, the Northern Hemisphere receives more heat than the Southern because the overturning circulation brings more heat into the Northern Hemisphere as opposed to the Southern. He also states that as a result, the extra heat is transferred to the tropical regions in the Northern Hemisphere, causing warm ocean water to be situated in the northern tropics. This warm ocean water is what eventually generates rain and thunderstorms, and because there is more warm water in the northern tropics, it is obvious that the tropical rain belt is moving northward. Due to global climate change, the circulation of ocean currents and ocean temperatures might adjust in favor of pushing the belt further north into the region of oscillation.
However, there is also the possibility that climate change will slow down ocean currents and circulation, which can change the present-day dynamic and send the rain belt to the south. Therefore, ocean circulation, ocean temperature, and the temperature of the earth are all attributing to the movement of the tropical rain belt. It is evident that the trend is northward and the belt is currently situated in the northern tropics, but the possibility of southward movement does exist. The northward movement does affect many countries and crops because the tropical rain belt is essential to food production in areas that rely on heavy precipitation.
The tropical regions will be affected most by the northward movement of the rain. The banana and coffee crops in Guatemala and Indonesia will become compromised by the loss of precipitation. In addition, the effects of a drier climate in Mexico could push the Mexican desert into southern portions of Texas, New Mexico and other areas in the southern U.S. Areas in the Middle East, Western America, and the Amazon rainforest risk the possibility of becoming drier and less humid. In contrast, the northward trend could bring more rain to areas in Asia already exposed to monsoons.
An increase of moisture in monsoon prone areas could be catastrophic as massive floods could follow the large amounts of rain added to preexisting rain from monsoons. Using geographical information, it is possible that the northward movement of the rain belt is already evident because of droughts in the western US, Syria and northern China. Although the possible adversarial effects of the movement can be devastating, the northward movement of the rain belt could bring an increase of rain to areas that have been decimated by droughts, which could prove to be very beneficial.