<span>-- The latitude at the northern end of the main runway at
Yakutsk Airport is 62.106° N. That point is roughly 460 miles
from the closest point on the seacoast.
-- The latitude at the northern end of the main runway at
Anchorage International Airport is 61.199° N. That point is
roughly 0.32 mile from the closest point on the seacoast.
Using these points of comparison, Yakutsk is 0.907° of latitude (62.7 miles)
more northerly than Anchorage, and Anchorage is roughly 460 miles closer
to the ocean than Yakutsk is.</span>
Answer: When the volume of the air increases, the air becomes less dense and rises. The rising, expanding air then creates an area of low-pressure.
Explanation: Edmentum
Weather is known over short periods of time and can be inaccurate, climate is figured out over long periods of time and effects a larger area
The atmosphere consists of 4 layers: the troposphere, stratosphere, mesosphere, and thermosphere. The troposphere is the lowest layer of the atmosphere. This is the layer where we live and where weather happens. Temperature in this layer generally decreases with height. The boundary between the stratosphere and the troposphere is called the tropopause. Above the tropopause lies the stratosphere. In this layer the temperature increases with height. This is because the stratosphere houses the ozone layer. The ozone layer is warm because it absorbs ultraviolet (UV) rays from the sun. The mesosphere is the layer above the stratosphere.This layer also contains ratios of nitrogen and oxygen similar to the troposphere, except the concentrations are 1000 times less and there is little water vapor there, so the air is too thin for weather to occur. The thermosphere is the uppermost layer of the atmosphere. In this layer the temperature increases with height because it is being directly heated by the sun.
I got this info from North Carolina Climate Office.
Hope this helps!!
Answer:
through increasing trade Brazil's long coastline helped the country to develop
