A continental slide is the new crust on the earth surface. It happens when two plates below the earth surfaces meets and the boundary became deep trenches.
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The continentality of Russia's climate increases as one travels east, with average temperature differences between the warmest and coldest periods in Eastern Siberia, for example, varying as much as 65 degrees Celsius (117 degrees Fahrenheit).
The continentality of Russia's climate increases as one travels east, with average temperature differences between the warmest and coldest periods in Eastern Siberia, for example, varying as much as 65 degrees Celsius (117 degrees Fahrenheit).
Ocean Currents and sea surface temperatures Altitude and Topography - mountain ranges Aspect Air masses and prevailing winds Lattitude Continentality Time of year - season Albedo Jet stream? Global warming?
Latitude: distance from the equator affects how directly sunlight reaches a location. Elevation: higher altitude generally results in lower temperatures due to decreased air pressure. Proximity to large bodies of water: moderates temperature by storing and releasing heat. Cloud cover: can block sunlight and insulate the Earth, affecting temperature. Urbanization: concrete and buildings absorb heat and can lead to higher temperatures in cities.
Continentality can be defined as large landmass. It results to severe temperature in Europe.
its simple
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continentality
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continentality
continentality
continentality
as the distansce from the sea increases, its moderating influence decreases and the people experience extreme weather conditions .this condition is known as continentality (i.e. very hot during summers and very cold during winters)
Continentality: the relationship between land masses (continents) and ocean bodies and the differences in temperature that are produced. Areas located in the interior of a continent are more likely to have greater temperature ranges and possibly drier conditions compared to maritime locations (land next to ocean). Because solar radiation heats land faster than water, Continentality causes greater extremes in both temperature and precipitation the farther inland an area is. This causes localized as well as global effects on weather patterns
The continentality of Russia's climate increases as one travels east, with average temperature differences between the warmest and coldest periods in Eastern Siberia, for example, varying as much as 65 degrees Celsius (117 degrees Fahrenheit).