warm oust air rises where it cools and condenses into clouds
Weather is The state of the atmosphere at a particular time and place.Weather is described in terms of variable conditions such astemperature, humidity, wind velocity, precipitation, and barometric pressure. Weather on Earth occurs primarily in the troposphere, orlower atmosphere, and is driven by energy from the Sun and therotation of the Earth. The average weather conditions of a regionover time are used to define a region's climate. The weather takes place in the Troposphere, the first layer of the atmosphere
By its heat energy content, yes. But the thin upper atmospheric layer called the thermosphere is hotter, considering the average temperature of the individual molecules there, which can exceed 1500 degrees Celsius.
Sunlight, oxygen and water. They use these to create chlorophyll through photosnythesis and that is their energy.
Convection
conduction
Weather is The state of the atmosphere at a particular time and place.Weather is described in terms of variable conditions such astemperature, humidity, wind velocity, precipitation, and barometric pressure. Weather on Earth occurs primarily in the troposphere, orlower atmosphere, and is driven by energy from the Sun and therotation of the Earth. The average weather conditions of a regionover time are used to define a region's climate. The weather takes place in the Troposphere, the first layer of the atmosphere
By its heat energy content, yes. But the thin upper atmospheric layer called the thermosphere is hotter, considering the average temperature of the individual molecules there, which can exceed 1500 degrees Celsius.
This is lame
Fusion
Sunlight, oxygen and water. They use these to create chlorophyll through photosnythesis and that is their energy.
Convection
Conduction :)
conduction
using it to create a different form of energy through resonance. or system's resonance frequencies, through amplitude oscillation. The system stores vibrational energy.
Yes mitochondria gives energy. It generates energy through respiration
The atmosphere can be divided into five layers based on temperature variations. The layer closest to the Earth is called the troposphere. Above this layer is the stratosphere, followed by the mesosphere, then the thermosphere. The upper boundaries between these layers are known as the tropopause, the stratopause, and the mesopause, respectively. Temperature variations in the four layers are due to the way solar energy is absorbed as it moves downward through the atmosphere. The Earth’s surface is the primary absorber of solar energy. Some of this energy is reradiated by the Earth as heat, which warms the overlying troposphere. The global average temperature in the troposphere rapidly decreases with altitude until the tropopause, the boundary between the troposphere and the stratosphere.
An electronic currant run through a copper coil will create a magnetic field.