Water circulates, and holds heat better than soil and rock. Therefore water will be warmer in the morning than surrounding ground (usually), and cooller in the late afternoon. When soil is frozen only the top few inches might thaw on a particularly warm day, while still water will tend to distribute the heat through the top few feet.
Sand and frost or snow raises the albedo of a surface, reflecting light and heat. Water tends to be darker, absorbing more heat. Dark, damp soil not overgrown has a low albedo, absorbing more heat yet.
A flat surface will absorb the most insolation since it has the maximum surface area exposed to the sun's rays. In contrast, a curved surface will have less surface area exposed to the sun, resulting in lesser insolation absorption over the same area.
The duration of insolation on March 21, also known as the spring equinox, is approximately 12 hours. This is because on the equinox, the sun is directly above the equator, resulting in nearly equal lengths of day and night worldwide.
Isobars show lines of equal atmospheric pressure, helping to identify areas of high and low pressure. Isotherms show lines of equal temperature, indicating temperature variations across a region. Both isobars and isotherms are used on weather maps to depict atmospheric pressure and temperature patterns respectively.
Lines making a circle around low pressure areas on a map indicate areas of equal pressure, known as isobars. These lines connect points of equal atmospheric pressure, with the closer the lines, the stronger the pressure gradient and potentially stronger winds. The direction in which the isobars are oriented can also indicate the wind direction around the low pressure system.
Isopleth lines, specifically isotherms, on a weather map indicate areas where the temperature is the same. These lines connect points of equal temperature, helping to visualize temperature patterns across the map.
A flat surface will absorb the most insolation since it has the maximum surface area exposed to the sun's rays. In contrast, a curved surface will have less surface area exposed to the sun, resulting in lesser insolation absorption over the same area.
The duration of insolation on March 21, also known as the spring equinox, is approximately 12 hours. This is because on the equinox, the sun is directly above the equator, resulting in nearly equal lengths of day and night worldwide.
no they are not unofficially But by constitution they are equal to while while they were not equal in 1960s.
Cut it from the top and straight down, and make 3 equal sized pieces.
Yes, it is the same number just written a little differently.
The area of the polygonal base, and the areas of each of its lateral faces (which need not be equal).The area of the polygonal base, and the areas of each of its lateral faces (which need not be equal).The area of the polygonal base, and the areas of each of its lateral faces (which need not be equal).The area of the polygonal base, and the areas of each of its lateral faces (which need not be equal).
The duration of insolation is the same everywhere on the days of the equinoxes - around March 20-21 for the vernal (spring) equinox and around September 22-23 for the autumnal equinox. During these times, the sun is directly above the equator, resulting in approximately equal day and night lengths worldwide.
yes
Yes.
Sum of the surface areas or each of its seven faces. Only the two pentagonal bases should have equal areas; there is no need for any of the other faces to have equal areas.
None! Coffee and adderall work very differently.
It means the areas are the same.