The answers would be: Article 2 uses a scientific claim because the author says the Earth is in a cooling cycle. Although Article 1 mentions evidence discovered by scientists, more research is needed about the data source to determine if the claim is scientific.
Water has a high heat capacity. This means it takes much energy (compared to other elements and compounds) to raise the temperatures of water by a degree. This, therefore, means that during the day, the land becomes hotter faster than the oceans. (The reason for sea breeze during the day). Likewise, during the night it takes much time for the water to lose the heat and drop its temperatures (compared to land – the reason for land breezes at night)
The answers would be: Article 2 uses a scientific claim because the author says the Earth is in a cooling cycle. Although Article 1 mentions evidence discovered by scientists, more research is needed about the data source to determine if the claim is scientific.
Water has a high heat capacity. This means it takes much energy (compared to other elements and compounds) to raise the temperatures of water by a degree. This, therefore, means that during the day, the land becomes hotter faster than the oceans. (The reason for sea breeze during the day). Likewise, during the night it takes much time for the water to lose the heat and drop its temperatures (compared to land – the reason for land breezes at night)
Evaporation from the seas is the essential system supporting the surface-to-air part of the water cycle. The considerable surface territory of the waters gives a chance to massive scale dissipation to happen. On a worldwide scale, the measure of water vanishing is equivalent to the standard of water conveyed to the Earth as precipitation. This varies topographically, however. Evaporation is more predominant over the seas than rainfall, while over the land, precipitation routinely surpasses vanishing. A high amount of the water that dissipates from the seas falls once again into the waters as precipitation.
Evaporation from the seas is the essential system supporting the surface-to-air part of the water cycle. The considerable surface territory of the waters gives a chance to massive scale dissipation to happen. On a worldwide scale, the measure of water vanishing is equivalent to the standard of water conveyed to the Earth as precipitation. This varies topographically, however. Evaporation is more predominant over the seas than rainfall, while over the land, precipitation routinely surpasses vanishing. A high amount of the water that dissipates from the seas falls once again into the waters as precipitation.
The warm ocean currents are responsible for the transportation of warm and moist air to the coastal region, whereas the cold ocean currents are responsible for carrying the cold and dry air to the nearby coastal areas.
Therefore, the region (1) will experience a cold and dry type of weather.
The stratosphere is the layer that is just above the troposphere and extends from a height of about 10 to 50 km above the ground surface. Here the temperature increases with the increasing height due to the presence of Ozone layer (O₃) that absorbs the incoming solar radiations.
Troposphere is the interior layer of the atmosphere that extends from the ground surface up to a height of about 10 km. Here, the temperature decreases with the increasing altitude. The air near the ground surface is compact and dense, due to which the temperature remains high. As the warm air rises up it interacts with the cold air that is situated over the warm air. Due to this, the air cools down and sinks to the bottom.
The warm ocean currents are responsible for the transportation of warm and moist air to the coastal region, whereas the cold ocean currents are responsible for carrying the cold and dry air to the nearby coastal areas.
Therefore, the region (1) will experience a cold and dry type of weather.
The stratosphere is the layer that is just above the troposphere and extends from a height of about 10 to 50 km above the ground surface. Here the temperature increases with the increasing height due to the presence of Ozone layer (O₃) that absorbs the incoming solar radiations.
Troposphere is the interior layer of the atmosphere that extends from the ground surface up to a height of about 10 km. Here, the temperature decreases with the increasing altitude. The air near the ground surface is compact and dense, due to which the temperature remains high. As the warm air rises up it interacts with the cold air that is situated over the warm air. Due to this, the air cools down and sinks to the bottom.
4
Get Answer
107
