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Watch a prototype of NASA's Volatiles Investigating Polar Exploration Rover, (VIPER) roll down a ramp to simulate its deployment on the lunar surface. <br/><br/>Credit: NASA
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Atmospheric pressure belts refer to the zones of high and low air pressure found at Earth's surface, primarily driven by the unequal heating of the planet by the sun. There are several key pressure belts:Equatorial Low-Pressure Belt (Intertropical Convergence Zone, ITCZ): Located near the equator, this belt experiences consistently low pressure due to intense solar heating, causing warm air to rise and create convectional rainfall.Subtropical High-Pressure Belts: Found around 30° latitude north and south of the equator, these belts result from descending air from the troposphere, creating stable, dry conditions. They are associated with deserts like the Sahara and Sonoran.Polar High-Pressure Belts: Near the poles, around 90° latitude, cold air descends and forms high-pressure zones. These regions are characterized by cold temperatures and dry conditions.Subpolar Low-Pressure Belts: These are found around 60° latitude north and south, where the polar air masses meet warmer air from the mid-latitudes. This mixing creates stormy weather and variable conditions.
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cyriak
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cyriak
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horizontal and vertical distribution of temperature,horizontal distribution of temperature,distribution of temperature,horizontal temperature distribution,regional distribution of temperature,temperature distribution on earth,temperature distribution,inversion of temperature,global distribution of temperature,vertical distribution of temperature,vertical and horizontal temperature,horizontal distribution,distribution of temperature class 11The horizontal distribution of temperature across Earth's surface is influenced by several factorsThe horizontal distribution of temperature across Earth's surface is influenced by several factors:<br/><br/>1. **Latitude**: Temperature generally decreases from the equator towards the poles due to the angle at which sunlight strikes the Earth's surface. This is why polar regions are colder than tropical regions.<br/><br/>2. **Altitude**: Temperature decreases with altitude due to the lapse rate, which averages about 6.5°C per kilometer. Higher elevations experience cooler temperatures than lower elevations at the same latitude.<br/><br/>3. **Ocean Currents**: Warm ocean currents can raise temperatures in coastal regions, while cold currents can lower temperatures. This effect is particularly noticeable along the western coasts of continents where warm currents flow poleward.<br/><br/>4. **Wind Patterns**: Wind direction and intensity can affect temperature distribution by redistributing heat. For example, westerlies can bring maritime air masses with moderate temperatures inland, while easterlies can bring cooler continental air
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cyriak
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cyriak
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Watch a prototype of NASA's Volatiles Investigating Polar Exploration Rover, (VIPER) roll down a ramp to simulate its deployment on the lunar surface. <br/><br/>Credit: NASA
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cyriak
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cyriak
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