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This title is printed to order. This book may have been self-published. If so, we cannot guarantee the quality of the content. In the main most books will have gone through the editing process however some may not. We therefore suggest that you be aware of this before ordering this book. If in doubt check either the author or publisher’s details as we are unable to accept any returns unless they are faulty. Please contact us if you have any questions.
The Earth's climate system consists of five interacting components namely atmosphere, hydrosphere, surface, biosphere and cryosphere, and influenced by various external forcing mechanisms. The most unstable component of the Earth's climate system is 'atmosphere's which has undergone significant changes since the evolution of the Earth (Baede et al., 2001). The present-day Earth's atmosphere is primarily composed of Nitrogen (78.08% by volume), Oxygen (20.95% by volume) and Ar (0.93% by volume). These gases do not interact with the incoming solar and outgoing terrestrial radiation significantly enough to alter the Earth's radiation balance. Water vapor (although variable, but typical volume mixing ratio is 1%) and some gases like CO2, O3, CH4 etc. (famously known as 'Greenhouse Gases',
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This title is printed to order. This book may have been self-published. If so, we cannot guarantee the quality of the content. In the main most books will have gone through the editing process however some may not. We therefore suggest that you be aware of this before ordering this book. If in doubt check either the author or publisher’s details as we are unable to accept any returns unless they are faulty. Please contact us if you have any questions.
The Earth's climate system consists of five interacting components namely atmosphere, hydrosphere, surface, biosphere and cryosphere, and influenced by various external forcing mechanisms. The most unstable component of the Earth's climate system is 'atmosphere's which has undergone significant changes since the evolution of the Earth (Baede et al., 2001). The present-day Earth's atmosphere is primarily composed of Nitrogen (78.08% by volume), Oxygen (20.95% by volume) and Ar (0.93% by volume). These gases do not interact with the incoming solar and outgoing terrestrial radiation significantly enough to alter the Earth's radiation balance. Water vapor (although variable, but typical volume mixing ratio is 1%) and some gases like CO2, O3, CH4 etc. (famously known as 'Greenhouse Gases',