Spring Tides. That is the High tide is very high and the low tide is very low. When the Sun, Earth and Moon are at 'right-angles to each other, then we have Neap Tides. The height range between high and low tides is much less than Spring Tides.
The poles, which are located at approximately 90 degrees latitude, receive the least amount of solar energy due to their extreme tilt away from the sun during certain times of the year. This results in prolonged periods of darkness and very low sun angles, leading to reduced solar energy reaching these regions.
Jaisalmer experiences high temperatures mainly due to its location in the Thar Desert, which receives intense sunlight. The desert landscape also lacks vegetation, which can help cool the surroundings through shade and evapotranspiration. Additionally, the region has low humidity levels, allowing temperatures to rise even higher during the day and drop significantly at night.
What happens when the clouds hang very low is that it becomes foggy. Fog is clouds that are very low to the ground and that are are made up of tiny water drops.
Albedo refers to the measure of how well a surface reflects sunlight. It is a unitless quantity, usually expressed as a percentage. A high albedo means a surface reflects a lot of sunlight, while a low albedo means it absorbs more sunlight.
It's so cold because it receives very little direct sunlight. Even when the sun shines all day, it is at a very low angle. Most of the radiation gets absorbed by the atmosphere before it is able to reach the earth.
The aphotic zone is located in the ocean below the depth of sunlight penetration. It is a deep, dark layer where sunlight cannot reach, resulting in very low to no light levels. Organisms in this zone have adapted to survive in complete darkness.
Because they get very low concentrations of sunlight.
The South Pole receives little solar radiation during the winter because of its high latitude, which causes the sun to stay very low or not rise above the horizon at all. This results in extended periods of darkness and low sunlight exposure during the winter months.
The side of a mountain that typically experiences lower temperatures is the north-facing side. This is because it receives less direct sunlight throughout the day, resulting in cooler temperatures compared to the south-facing side, which receives more direct sunlight and tends to be warmer.
Uranus receives very little sunlight due to its distance from the Sun, resulting in low levels of light on its surface. However, the planet does have its own unique and faint glow from its atmosphere reflecting sunlight.
The polar regions, specifically the Arctic and Antarctic, receive very little solar energy because of their extreme latitudes and long periods of darkness during winter months. The angle of incidence of sunlight is very low, resulting in reduced heating and energy absorption.
The Antarctic region is much colder than the Atlantic region for two main reasons: 1. The Antarctic receives a lot less sunlight. The earth's axis is on a tilt, which causes seasons as the earth travels around the sun. During the antarctic winter, much of the region goes without sunlight for many months at a time. 2. The Antarctic region is at a very low angle relative to the sun's light. The equator receives the sun's light at about a 90 degree angle, or straight on. This means the full force of the light hits the surface of the earth. At the poles however, the low angle means the light hits the surface of the earth with much less intensity, so what little sunlight the Arctic gets isn't very strong.
There are many reasons places can flood but flooding in Bangladesh is terrible this is because of:-The monsoon rainfalls-The low lying land -so the water can not drain-And also in the summer when the snow melts of the mountains and overflows the rivers!
The equator receives approximately 12 hours of sunlight during the spring. Due to the tilt of the Earth's axis, the amount of sunlight received at the equator remains fairly consistent throughout the year.
The shaded side of the mountain tends to experience lower temperatures as it receives less direct sunlight and, therefore, less heat. This phenomenon is known as the rain shadow effect.
Lake Tanganyika is very near the equator (3.3 to 8.9 degrees south latitude), in tropical Africa, so it receives considerable sunlight despite having about the same day length year-round. However, cloud cover is much greater in the summer "wet" season (November to April). The temperatures in the rift valley are typically from the high 60s to the low 80s (Fahrenheit).