Answer:
Baker (plaintiff) was a Republican living in Shelby County, Tennessee. The Tennessee Constitution required that legislative districts be redrawn every ten years to adjust for changes in population. Baker brought suit against Carr (defendant), Secretary of State in Tennessee, in his official capacity alleging that because Tennessee had not actually redistricted since 1901, the urban Shelby County district had ten times as many residents as did the more rural districts. As a result, Baker argued that rural votes counted more than urban votes, and that he was thus denied equal protection of the laws. The State of Tennessee argued that legislative districting issues were not judicial questions but political questions, and were thus not capable of being decided by the courts based on the Constitution’s prohibition on the Court’s deciding political questions.
Explanation:
It a b and c hope it helps you
The troposphere is the lowest layer of Earth's atmosphere, and is also where nearly all weather conditions take place. It contains approximately 75% of the atmosphere's massand 99% of the total mass of water vapor and aerosols.[2] The average height of the troposphere are 18 km (11 mi; 59,000 ft) in the tropics, 17 km (11 mi; 56,000 ft) in the middle latitudes, and 6 km (3.7 mi; 20,000 ft) in the polar regions in winter.
The lowest part of the troposphere, where friction with the Earth's surface influences air flow, is the planetary boundary layer. This layer is typically a few hundred meters to 2 km (1.2 mi; 6,600 ft) deep depending on the landform and time of day. Atop the troposphere is the tropopause, which is the border between the troposphere and stratosphere. The tropopause is an inversion layer, where the air temperature ceases to decrease with height and remains constant through its thickness.[3]
The word troposphere is derived from the Greek tropos (meaning "turn, turn toward, change") and sphere (as in the Earth), reflecting the fact that rotational turbulentmixing plays an important role in the troposphere's structure and behaviour. Most of the phenomena associated with day-to-day weather occur in the troposphere.
