CLIMATE & BIOMES
  
Continental and Marine Climates

What do you think? Can we expect all places at the same latitude to have the same temperature and precipitation?


Why or why not?






Using the GLOBE database and graphing tools you can display and examine different maps from different regions.

Temperatures vary greatly from place to place on the Earth. Among the factors which produce variations in the temperature are: altitude, latitude, land and sea, wind and ocean currents, clouds and relief.

One of the most important factors that affect temperature, is latitude. Latitude has a powerful influence in determining seasonal conditions and the annual patterns of environmental and climatic parameters e.g. precipitation and temperature. People studying our planet's climate have found out that the temperature and precipitation amounts differ at the same latitude.



Why?



The size of a continent affects both the temperature range and the amount of moisture in the interior. The larger the continent, the larger the effect. Interior climates are defined as continental and windward coastal climates as marine. Due to the moderating effect of water, sites having a marine climate are considered comparatively mild.

In order to characterize marine and continental climates it is necessary to look at the climatic conditions of different places found at the same latitudes.

The GLOBE software can create maps for you. Please follow the instructions:
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Background
Climatic Conditions at Same Latitude

Why, on a sunny summer's day is the land much hotter than the sea?


Why are the average precipitation amounts different at the same latitude?

Climatic conditions associated with continental areas are characterized by marked temperature contrasts between night and day and from season to season. The sun's "rays" strike the Earth's surface providing energy in the form of heat. Some of this energy re-radiates back into the atmosphere and warms the air. Some is absorbed by a very thin layer of the Earth's crust. This thin layer warms up very quickly. It also cools down just as rapidly. However, in the sea, solar radiation penetrates much deeper and further. The heat energy spreads through a greater volume. The result is that the sea may warm up slower than the land but it retains its heat for longer. The earth in contrast, gains and looses heat more quickly than the sea.

Our planet is a water planet. Like atmospheric air, the waters of the oceans are mixed and circulated. One of the key roles of water on Earth is to transfer heat from the tropics to higher latitudes. This is done both by the movement of ocean waters (currents) and by the movement of water in the atmosphere. Warm water from the tropics flows towards the poles, and cold water from the polar regions flows towards the equator.

Winds blowing over warm ocean currents are warmed. They also pick up moisture from the water surface. When these moist winds reach the land, they bring rain. Marine climates are characterized by small annual and diurnal temperature variation and by copious rainfall on the windward side of coastal highlands and mountainous islands. Coastal regions tends to have more stable temperatures throughout the year.

Not all coastal environments have the same precipitation patterns. For example, the Atlantic and Pacific coasts of the North American continent have different current patterns and prevailing winds that result in different kinds of marine climates.

However, both these marine climates have moderate temperature extremes and have considerable moisture in the air.