The climate of India is complex, with a wide range of weather conditions over a large geographic area and varying topography, making generalisations difficult. India has six distinct climatic subtypes, ranging from dry deserts in the west to alpine tundra and glaciers in the north, and wet tropical areas with rain forests in the southwest and island territories, according to the Koppen climate classification. It is one of the world’s most climatically diverse countries, with several regions having significantly different microclimates.
The country’s meteorological agency maintains the global pattern of four seasons, with some local adaptations: winter (January and February), summer (March, April, and May), monsoon (rainy) season (July to August), and a post-monsoon period (October to December).
Climatic Controls
Climate is defined as the sum of weather conditions and fluctuations over a long period of time throughout a vast area. Weather refers to the state of the atmosphere above a given region at any given time. The weather may change throughout the day, but the climate of a country remains consistent over many years.
A vast body of evidence suggests that human activity, such as agriculture and industrialization, causes unintentional weather change. Acid rain harms freshwater lakes, plants, and structures because it is caused by industrial sulphur dioxide and nitrogen oxide emissions into the atmosphere. Air quality and visibility are both harmed by anthropogenic pollutants.
The long-term consequences of accidental weather manipulation could endanger ecosystems, natural resources, food and fibre production, economic growth, and human health.
Drought, extreme temperatures, flooding, high winds, global warming, and severe storms are expected to become more common as a result of climate change caused by human activities that release greenhouse gases into the atmosphere. “Climate Change” is a term that is widely used to describe global warming.
Factors for Climate Control
Factors of climatic control are the permanent factors that affect the general type of the climate of any area on Earth. There are six climatic control elements listed below:
Latitude
Due to the curvature of the planet, the amount of solar radiation received varies with latitude, resulting in a decrease in temperature from the equator to the poles.
Effect of Latitude
Due to the curvature of the planet, the amount of solar radiation received varies with latitude, resulting in a decrease in temperature from the equator to the poles.
Altitude
Once one rises above the Earth’s surface, the air gets less thick and the temperature drops. The hilly regions are much cooler in the summer as a result of the temperature change caused by the altitude.
Pressure and Wind System
Both latitude and altitude influence an area’s pressure and wind system, as well as its temperature and rainfall pattern.
Distance from the Sea
As the distance from the sea increases, it has a moderating effect on the climate. It indicates that as the distance from the sea increases, the weather conditions get more intense as the moderating impact diminishes. Continentality is the term for this. The weather gets extremely hot in the summer and extremely frigid in the winter in this situation.
Ocean Currents
Ocean currents, as well as onshore winds, influence the climate of coastal places. For example, if the winds are onshore currents flowing warm or cold, any coastal location will be cooled and warmed.
Relief Features
Relief has an essential function in determining the climate of every location. Because high mountains operate as a barrier for cold and hot breezes, they may create precipitation if they are high enough and in the path of rain-bearing winds. As a result, the leeward side receives less rain or is almost completely dry.
Role of Atmosphere in Climatic Control
The atmosphere shields us from cosmic rays and radiation from space. The ozone layer in the atmosphere protects the globe from harmful UV rays. The majority of the destructive effects of cosmic rays, gamma rays, and X-rays are blocked by dense layers of molecular gases.
Tonnes of space debris collide with the Earth every day. The molecules in the atmosphere destroy them before they reach the earth. The water vapour condenses and falls as rain, providing the earth with a life-sustaining resource. If there had been no atmosphere, the water would have boiled out into space or remained frozen.
Conclusion
The climate of India is complex, with a wide range of weather conditions over a large geographic area and varying topography, making generalisations difficult.Climate is defined as the sum of weather conditions and fluctuations over a long period of time throughout a vast area. Weather refers to the state of the atmosphere above a given region at any given time. The weather may change throughout the day, but the climate of a country remains consistent over many years.