The low latitudes are generally warm lands.
Average temperatures in UK are warmer at lower latitudes and colder at higher latitudes.
Tussock grasslands occur at various latitudes.
At higher latitudes, the winds blow eastward at slower speeds.
They were named by the sailors who first entered these latitudes.
Although summers are brief at high latitudes, the days of summer are long.
In the higher latitudes, Earth gives off more heat than it receives from the Sun.
Projections other than the Mercator are also used, especially in very high latitudes.
During the short summer season, the wind systems of the polar latitudes are greatly weakened.
In contrast, at low latitudes ice is unstable, and any ice present in the ground would tend to sublime into the atmosphere.
Wetter areas on other continental blocks in higher latitudes of the Northern Hemisphere began to form coal swamps during this time.
Regions in high latitudes, both north and south, get less insolation and are therefore usually colder than regions in low latitudes.
Nearly all major taxonomic groups have fewer species of animals and plants in the taiga than they have in other terrestrial ecosystems at lower latitudes.
The effect of latitude is evident in the large north-south gradients in average temperature that occur at middle and high latitudes in each winter hemisphere.
Above that level, a reversal of the horizontal temperature gradient occurs, which produces a reduction in the wind speeds of the jet stream at high latitudes.
As in the North Atlantic, the weather usually is settled and fine in the latitudes of high pressure but is unsettled and stormy in the higher latitudes of the westerlies.
In addition, since the mid-latitudes also become colder during the winter, while tropical temperatures remain relatively unchanged, the westerly jet stream approaches latitudes of 30° during the colder season.
Within the belts of the westerly winds, cold easterly winds from polar regions meet the warm westerly winds of the middle latitudes, causing the formation of the traveling depressions characteristic of middle latitudes.
As a result, the solar energy is spread over a greater area at high latitudes than at low latitudes, and less solar energy reaches Earth’s surface at high latitudes because more is absorbed and reflected by the atmosphere.
In contrast, during the summer at high latitudes, the troposphere warms significantly as a result of the long hours of daylight; however, owing to the oblique angle of the sunlight near the poles, the temperatures there remain relatively cool compared with middle latitudes.
latitudes
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