The influence of the distribution of seas and land on the terrestrial climate has given rise to two extremely different climates, namely the continental climate and the oceanic climate.
The most notable characteristic of the continental climate is its rapid and significant changes, with large daily and annual temperature differences. In the annual temperature changes, the warmest season in continental climate occurs in July and the coldest season in January. The temperature rises quickly in spring and cools quickly in autumn. Generally, the temperature in spring is higher than in autumn. In the diurnal variation, the highest temperature appears earlier, generally between 1 and 2 p.m.; the lowest temperature usually appears at dawn. Another important characteristic of the continental climate is the low precipitation and its seasonal and regular distribution.unequal. Areas under the influence of the continental climate have low relative humidity and are generally arid and semi-arid areas. Rainfall is generally less than 400 mm, and in some areas it is even less than 50 mm.
Compared to the continental climate, the main characteristic of the oceanic climate is that the annual and daily temperature changes are small. In oceanic climate, the highest temperature usually occurs in August and the lowest temperature occurs in February. the temperature changes later than on the continent. The seasonal distribution of precipitation is relatively uniform, with many days of precipitation and low intensity. The weather is cloudy and foggy, with high humidity all year round. In terms of annual temperature changes, autumn is cooler than spring, which is an important characteristic of the western climate.eanic.
The distribution of sea and land will also have some impact on atmospheric pressure and wind. Monsoons form primarily due to temperature differences that exist between adjacent continents and oceans. The atmospheric pressure distribution changes with the temperature distribution. In summer, the continent is a source of heat and the ocean a source of cold. Therefore, land pressure is low and sea air pressure is high, causing wind to blow from the ocean to the ocean. the continent. In winter, the ocean is a source of heat, the continent is a source of cold, and sea air pressure is low, land pressure is high, so the wind blows from land to the ocean. As wind direction changes, Earth's climate also changes.
In addition, the distribution of land and sea also affects ocean circulation and has an impact indirectly on the climate. For example, about 3,000 years ago, South America and Antarctica, which were originally connected, separated and drifted, and an ocean current around Antarctica formed between both. The ocean current originally coming from the tropics was cut off and could no longer function. transport thermal energy to the Antarctic continent from sea areas.
Your problem is too big. The ocean plays a huge role in the climate. It is recommended to consider these aspects.
The first is energy. The enormous thermal capacity of the oceans stores much more thermal energy than the land and the atmosphere. Balances summer and winter energy. Ocean currents transport heat from low latitudes to high latitudes. “The Day After” is about that. Sea surface temperature also has an important influence on the atmosphere, and ENSO is one of them.
Mores, the breaking of ocean waves produces aerosols in the atmosphere. Carbon dioxide dissolves in water, making the ocean a carbon sink. Marine algae provides more than half of the world's oxygen. Concerning radiation, the reflection and absorption of solar radiation by the ocean greatly affects the climate.