The relationship that you expect to find between the air temperature and dew point temperature at ground level if the area is covered by fog is the temperatures of th air and the dew point would be very close in value.
The relationship that you expect to find between the air temperature and dew point temperature at ground level if the area is covered by fog is the temperatures of th air and the dew point would be very close in value.
At a height of 500 meters up a mountain, the temperature is generally expected to be cooler than at sea level. As a rule of thumb, the temperature decreases by approximately 6.5 degrees Celsius for every 1,000 meters of elevation gain in the troposphere. Therefore, if the base temperature at sea level is known, you can estimate a drop of about 3.25 degrees Celsius at 500 meters. However, local factors such as weather conditions and geographical features can also influence the actual temperature.
On average, the temperature decreases by around 3.5°F for every 1,000 feet increase in elevation, known as the lapse rate. At 8,000 feet altitude, you can expect the temperature to be around 28°F cooler than at ground level, so it would be approximately 42°F at that height if the ground temperature is 70°F.
The smallest variation in temperature from year to year and from month to month is typically experienced in tropical coastal regions. These areas, such as those near the equator, benefit from a stable climate characterized by consistently warm temperatures and minimal seasonal changes due to their proximity to large bodies of water, which moderate temperature fluctuations. Additionally, ocean currents and prevailing winds contribute to this temperature stability.
What would you expect to find composite volcanoes on Mars? Explain why.
The relationship that you expect to find between the air temperature and dew point temperature at ground level if the area is covered by fog is the temperatures of th air and the dew point would be very close in value.
In areas covered by fog, the air temperature is typically close to the dewpoint temperature. This is because fog forms when the air temperature cools to the dewpoint temperature, causing water vapor in the air to condense into tiny water droplets that make up the fog.
When an area is covered by fog, the air temperature and dew point temperature are typically very close to each other, often within a degree or two. This is because fog forms when the air becomes saturated with moisture, causing the dew point to rise to near the current air temperature. As a result, you would expect to find a minimal difference between the two temperatures in foggy conditions.
When an area is covered by fog, the air temperature and dew point temperature are typically very close to each other, often within a few degrees. This is because fog forms when the air is saturated with moisture, leading to high relative humidity. As a result, the air temperature approaches the dew point temperature, indicating that the air is nearly at its maximum capacity to hold moisture. Thus, you would expect to find a small difference between the two temperatures.
When an area is covered by fog, the air temperature is typically very close to the dew point temperature at ground level. This is because fog forms when the air is saturated with moisture, which occurs when the temperature drops to the dew point. As a result, the air temperature and dew point temperature can be nearly equal or within a few degrees of each other, indicating high humidity and the presence of fog.
*Typically that is the relationship between service and cost.
The correlation between cricket chirps and the temperature is very approximate.
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You would expect the daily temperature range to be higher in a continental climate compared to a maritime climate. Continental climates tend to have larger temperature variations between day and night due to the absence of moderating effects from large bodies of water.