Factors that influence the overall climate are the radiation from the Sun, the tilt of Earth's axis, the geography of the oceans and continents, the average cloud cover, and the amount of greenhouse gasses in the atmosphere.
Related to the cycle of sea temperatures are the El Niño / La Niña events and the long-term changes due to Earth's orbit are called the Milankovitch cycles.
Factors that contribute to Earth's climate include the concentration of greenhouse gases in the atmosphere, the amount of solar radiation reaching Earth, the distribution of land and water on the planet, and ocean currents. These factors interact in complex ways to determine the temperature and weather patterns that we experience.
The absorption of thermal energy from the ground to the air can lead to an increase in temperature at the Earth's surface. This process can affect weather patterns, contribute to the greenhouse effect, and influence the overall climate of a region.
The tundra formed through a combination of factors including glaciation, weathering, and erosion over millions of years. Climate conditions in these regions are characterized by low temperatures, short growing seasons, and permafrost which all contribute to the unique tundra landscape.
Predicting how Earth's climate will be affected by changes in the atmosphere is difficult because the climate system is complex and influenced by numerous interacting factors, making it challenging to model accurately. Additionally, human activities can introduce unpredictable variables that further complicate predictions. The long timescales and nonlinear dynamics of the climate system also contribute to the uncertainty in predicting future climate outcomes.
Individual activities or personal choices do not directly control the climate. Climate is primarily influenced by natural factors such as solar radiation, volcanic activity, and the Earth's orbit, as well as human activities that release greenhouse gases into the atmosphere.
it depends on air pressure and where is place located (tropical-hot climate etc
each biome has a certain climate and organisms
earths tempertures
temperarure, precipitation, and nitromonoxide
Factors that contribute to Earth's climate include the concentration of greenhouse gases in the atmosphere, the amount of solar radiation reaching Earth, the distribution of land and water on the planet, and ocean currents. These factors interact in complex ways to determine the temperature and weather patterns that we experience.
Changes in the Earth's climate are primarily caused by natural factors, such as volcanic eruptions, solar radiation variations, and ocean currents, as well as human activities, particularly the burning of fossil fuels, deforestation, and industrial processes. These activities increase greenhouse gas concentrations in the atmosphere, leading to global warming and altering weather patterns. The resulting impacts include rising sea levels, more extreme weather events, and shifts in ecosystems and biodiversity. Overall, both natural and anthropogenic factors contribute to ongoing climate change.
The absorption of thermal energy from the ground to the air can lead to an increase in temperature at the Earth's surface. This process can affect weather patterns, contribute to the greenhouse effect, and influence the overall climate of a region.
The tundra formed through a combination of factors including glaciation, weathering, and erosion over millions of years. Climate conditions in these regions are characterized by low temperatures, short growing seasons, and permafrost which all contribute to the unique tundra landscape.
Predicting how Earth's climate will be affected by changes in the atmosphere is difficult because the climate system is complex and influenced by numerous interacting factors, making it challenging to model accurately. Additionally, human activities can introduce unpredictable variables that further complicate predictions. The long timescales and nonlinear dynamics of the climate system also contribute to the uncertainty in predicting future climate outcomes.
The Earth's orbit affects its temperature primarily through variations in solar radiation received at different times of the year due to its elliptical shape and axial tilt. These factors create seasonal changes, influencing climate patterns. Over long periods, shifts in the Earth's orbit, known as Milankovitch cycles, can lead to significant climate changes, contributing to glacial and interglacial periods. Ultimately, these orbital variations play a crucial role in regulating the Earth's overall climate and temperature.
The factors include, Reflectivity of the area, Topography, Climate, Cloud cover, Vegetation, and Latitude.
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