Answer:
The correct option is: dew point temperature
Explanation:
Dew point refers to the temperature of the air when it is saturated with water vapor. The dew point temperature is dependent on the humidity in the air. It is <u>directly proportional to humidity and moisture content in air</u>. <u>Therefore, a lower dew point means lower moisture content. </u>
When the air is cooled beyond its dew point, the water vapour in the air condenses to liquid water, called dew.
Maybe there's an app for that? Some kind of time lapse app? Or maybe set up a magnifying glass or a crystal ball on a stand and a piece of paper under it. As the sun passes, it will might burn a line on the page. As to how you would read this line, you would need some kind of measurement system - maybe do a baseline the day before and use you watch to record start and finish times.
Answer:
C. Ageing infrastructure as exceptionally expensive to maintain.
Explanation:
Near the South Nation River lies the Galop Canal, the historical predecessor to the St. Lawrence Seaway. Galop Canal ran 12 kilometers from Iroquois to Cardinal. The nature of life along the St. Lawrence banks began to change and newer, larger, locks were built to ship larger amounts of cargo from the Great Lakes.
Answer:
LA = 20π cm²
Explanation:
Given the following data;
Radius, r = 4 cm
Height = 3 cm
To find the lateral area (LA) of a cone;
First of all, we would determine the slant height by applying Pythagorean' theorem.
Hypotenuse² = opposite² + adjacent²
Where;
Hypotenuse is the slant height.
Opposite is the height of the cone.
Adjacent is the radius of the cone.
Substituting into the expression, we have;
l² = 3² + 4²
l² = 9 + 16
l² = 25
Taking the square root of both sides, we have;
l = √25
l = 5 cm
Next, we find the LA using the formula;
LA = πrl
Where;
r is the radius of the cone.
l is the slant height of the cone.
Substituting into the formula, we have;
LA = 4 * 5 * π
LA = 20π cm²
Rockslides on hills and mountains are created as gravity erodes and deposits rocks. In the desert, the deposition patterns of the wind creates sand dunes. Streams create deltas when they deposit sand and sediment at their mouths, where the water slows to meet the ocean.
