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Ocean currents:  search and ocean currents have different  temperature is that well either  warm or cool the air above it  which changes the coast  temperature

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What these factors are is ocean currents, topography, vegetation and prevailing winds

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include latitude.
elevation.
Nearby water..
Ocean currents.
Topography.
Vegetation.
Prevailing winds.

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The 6 major factors is elevation, latitude, large bodies of water, ocean currents, topography, prevailing and seasoning winds. A distance from the equator affects the climate of a place. At the poles from the energy from sun reaches earth lower surface and passes through a thicker layer of atmosphere which means the climate is cooler further from equator.

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Different climates have different conditions and strengths.

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The climate of any place is influenced by a host of interacting factors

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Weather is the temperature, whether or not it is sunny or cloudy, etc for a particular day.

Climate is the ANNUAL (year) pattern of weather for a particular place or region (when looking at all daily weather combined over the course of a year).

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Nearby water

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Distance from the sea

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Weather over a period of time and area.

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Ocean currents, the shape of the land

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It affects it by a place in a different way when the equator receive  more sunlight. And further from the equator less sunlight you receive. other factors the climate receive other than latitude is closeness to the sea elevation.

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v

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The shape of the land

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prevailing winds

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The closer to the  equator the hotter it is there

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Find out what a chinook is?

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The dominant air currents that affect climate are known as prevailing winds. For example, warm winds that travel over water tend to collect moisture as they travel; the water vapor in the air will condense as it moves into colder climates, which is why temperate ms in coastal areas often receive heavy rainfall.

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The dominant air currents that affect climate are known as prevailing winds. For example, warm winds that travel over water tend to collect moisture as they travel; the water vapor in the air will condense as it moves into colder climates, which is why temperate ms in coastal areas often receive heavy rainfall.

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Sea level is the standard measure of 0.

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High and low grounds💯

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Air pressure and air temperature decrease with altitude.

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High and low grounds and the winds etc....💯💯

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Every 1,000 feet higher, temperature drops by 4°f

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Bodies of water affect climate because water heats up and cools down slower than land making more moderate climates with smaller temperature ranges.

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The closer you are to the equator the more sunlight you recieve, the further away the less sun, making it cooler in Canada than in Florida or Mexico

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how does latitude affect climate - Bing images

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World Climate Different Climate Zones Climate Factors Factors That Affect Climate Factors Affecting Climate Latitude and Climate How Does Elevation Affect Climate Factors That Influence Climate Diagram of Zones of Latitude Factors That Affect Weather Latitude and Climate Map How Does Topography Affect Climate How Does Altitude Affect Climate How

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Mountains affect climate by blocking wind and receiving more rainfall than low-lying areas. As air is forced over higher ground, it cools, causing moisture to condense and fall as rain. The higher a location is above sea level, the colder it is.

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oceans, seas, and large lakes

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For every 1,000 meters above sea level, temperatures decrease by 9.8°C

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A warm dry wind which blows down the east side of the Rocky Mountains at the end of winter.
Chinook winds, or simply Chinooks, are föhn winds in the interior West of North America, where the Canadian Prairies and Great Plains meet various mountain ranges, although the original usage is in reference to wet, warm coastal winds in the Pacific Northwest.

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Large bodies of water such as the oceans ,seas and also large lakes affect climate of the area

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wind currents are formed by a process known as convection when pressure and convection come together they create an air flow that flows to lots of different areas which then affects the climate

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The currents from water from a warmer region brings warm air to land it hits and same with cold currents

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The higher up you go, the air is less dense and the molecules are farther apart. This affects the climate because when the molecules are closer together, they are more likely to collide. When molecules collide, they give off heat. This is why it gets colder when you go up higher. The air is less dense and the molecules won’t collide as often, and won’t give off as much heat.

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See appendix on page 241 - map of wind systems

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Large lakes and oceans and when the water heats up and cools down slower than land making and climate with smaller temperature🇬🇭🇷🇪

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The air over the hotter parts of the earth is warmed by the heat from the surface of land or water.

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The Coriolis force is the affect of the earths rotation on its axis from west to east. This makes the wind in the northern hemisphere seem like is is swerving to the right and the winds that are in the Southern Hemisphere seem like they are swerving  to the left.

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cycle of the chinook

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Large bodies of water such as oceans, seas, and large lakes affect the climate of an area. Water heats and cools more slowly than land. Therefore, in the summer, the coastal regions will stay cooler and in winter warmer. A more moderate climate with a smaller temperature range is created.

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Large bodies of water such as oceans, seas, and large lakes affect the climate of an area. Water heats and cools more slowly than land. Therefore, in the summer, the coastal regions will stay cooler and in winter warmer. A more moderate climate with a smaller temperature range is created.

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Latitude is latitude

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Altitude is part of the reason mountains have snowcap. Normally, we would think the top of a mountain it the warmest point because heat rises & it is closer to the sun, but actually, the coldest point of a mountain is at the top. The higher you climb up a mountain, the thinner the atmosphere gets. This is because the air pressure decreases with altitude. Even though warm air rises, when it rises, it also expands and cools. When it expands and cools, it can’t take up and hold as much heat as it can at the bottom of the mountain. Also, cooler temperatures mean less evaporation. Evaporation means more moisture. More moisture can lead to more rain. Or at the top of the mountains, snow. This is why mountains have snowcaps.

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Cold  currents that originate in the polar regions bring cold air to the equator and warm currents which originated in the tropics bring warm air to cooler regions.

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Latitudes affect the climate of a place in different ways. First, places close to the equator receive more sunlight, as such, the farther you are from the equator, the less sunlight you receive. ... Other factors that affect the climate of the place other than latitudes include; Closeness to the sea, elevation etc.

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Mountains affect climate by blocking rain from one side of the mountain so one side would be dry and the other all rainy

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Since the equatorial areas are hot and the polar areas are cold we might expect the winds to always move along the surface of the earth from the poles to the equator this does not happen for 2 main reasons: the earth rotates, and it has an unequal distribution of land and water around its surface

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The temperature of the water affects the temperature of the air which effects the climate in areas.

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Ocean currents

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The higher you are from sea level, also affects vegetation and wildlife. For example, deserts are tend to be hotter and closer to sea level than mountains.

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The rain falls on the windward side of the mountain because it’s on higher ground on the other side of the mountain it’s dry because it’s a low lying area. The top of the mountain will be cold because the higher location above the sea leve the colder it will be.

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This diagram explains how the heat stays longer when there is less altitude. The molecules are more spread out which makes it easier for heat to escape.

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Mountain barriers influence climate Patterns. When moisturebeariing winds meet mountains, they move up the windward sides of these barriers. As the air rises, it cools. Condensation produces clouds, and then rain. By the time the air reaches the tops of the mountains it has released most of its moisture.