Cover of: Researches on solar heat and its absorption by the earth

Researches on solar heat and its absorption by the earth"s atmosphere

a report on the Mount Whitney expedition
  • 242 Pages
  • 1.14 MB
  • 3034 Downloads
  • English
by
Government Printing Office , Washington
Solar radiation, Infrared spectra, Actinometer, Whitney, Mount (Ca
Statementby S.P. Langley.
SeriesProfessional papers / Signal Service -- No. 15, Professional papers (Signal Service) -- No. 15.
Classifications
LC ClassificationsQC911.L26
The Physical Object
Pagination242p. :
ID Numbers
Open LibraryOL18254419M
LC Control Number05008118

Researches on solar heat and its absorption by the earth's atmosphere: a report on the Mount Whitney expedition [Langley, S P. ] on *FREE* shipping on qualifying offers. Researches on solar heat and its absorption by the earth's atmosphere: a report on the Mount Whitney expedition.

Get this from a library. Researches on solar heat and its absorption by the earth's atmosphere: a report of the mount Whitney expedition. [Samuel Pierpont Langley;]. NASA Images Solar System Collection Ames Research Center.

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Video. An illustration of an audio speaker. Audio An illustration of a " floppy disk. Full text of "Researches on solar heat and its absorption by the earth's atmosphere: a report on the Mount Whitney expedition. From a limited number of cloudy sky optical path observations, the atmospheric (O2)2 absorption is estimated to account for an additional solar heating of about W m−2 globally averaged.

The absorption of solar energy heats up our planet’s surface and atmosphere and makes life on Earth possible. But the energy does not stay bound up in the Earth’s environment forever. If it did, then the Earth would be as hot as the Sun. Instead, as the rocks, the air, and the sea warm, they emit thermal radiation (heat).

Solar radiations while passing through the earth’s atmosphere are subjected to the mechanism of atmospheric absorption and scattering.

A fraction of the radiation reaching the earth’s surface is reflected back into the atmosphere and is subjected to these atmospheric phenomenon again, the remainder is absorbed by the earth’s surface.

Due to the Earth’s atmosphere, solar radiation is attenuated by phenomena such as atmospheric absorption and scattering, as well as cloud reflectance, before reaching the land surface (Section ). Generally, when solar radiation penetrates the atmosphere, water vapor and carbon dioxide absorb the infrared energy, while the ozone layer.

Climate - Climate - Solar radiation and temperature: Air temperatures have their origin in the absorption of radiant energy from the Sun. They are subject to many influences, including those of the atmosphere, ocean, and land, and are modified by them. As variation of solar radiation is the single most important factor affecting climate, it is considered here first.

Above: (Left) The Earth’s surface, warmed by the Sun, radiates heat into the atmosphere. Some heat is absorbed by greenhouse gases like carbon dioxide and then radiated to space (A).

Some heat makes its way to space directly (B). Some heat is absorbed by greenhouse gases and then radiated back towards the Earth’s surface (C). All living things need some of the gases in air for life support.

Without an atmosphere, Earth would likely be just another lifeless rock. Earth’s atmosphere, along with the abundant liquid water at Earth’s surface, are the keys to our planet’s unique place in the solar system. Much of what makes Earth exceptional depends on the atmosphere.

The heat budget: When the sun shines on Earth, part of it is reflected back by the outer atmosphere to space, part of it is absorbed by the atmosphere, and part by the surface of the Earth.

Both those quantities of heat that are absorbed by the Earth and the atmosphere are irradiated back to space, so that the total amount of heat that comes to. warms the Earth, but also means that the sun is not directly heating the troposphere.

Rather, this solar energy warms the Earth, and the Earth emits its own energy to space. Because the surface of the Earth is much cooler than the surface of the Sun, the Earth emits most of its energy at longer wavelengths (i.e., lower energy radiation).

Almost all. Although solar flares, and associated coronal mass ejections, can bombard Earth’s outermost atmosphere with tremendous amounts of energy, most of that energy is reflected back into space by the Earth’s magnetic e the energy does not reach our planet’s surface, it has no measurable influence on surface temperature.

Atmospheric Radiation and Earth’s Climate. Let’s first look at the general energy balance—the radiative equilibrium—of the Earth system (see figure below).The solar irradiance is essentially composed of parallel radiation beams (or radiances) that strike half the globe.

­Why does the air absorb this home-brewed radiation on the rebound instead of the fresh solar energy. Well, a solar-charged Earth emits long-wave radiation. While water vapor and carbon dioxide molecules merely allow the passage of incoming short waves, they absorb Earth's long waves, heating the atmosphere from the ground up.

K.R. Lang, in Encyclopedia of Geology, Basic Properties of the Solar Wind.

Description Researches on solar heat and its absorption by the earth"s atmosphere EPUB

The tenuous solar atmosphere expands out in all directions, filling interplanetary space with a ceaseless wind that is forever blowing from the Sun. This solar wind is mainly composed of electrons and protons, set free from the Sun's abundant hydrogen atoms, but it also contains heavier ions and magnetic fields.

Atmosphere Table of Contents Introduction 3 Discussion 4 Conclusion 8 References 10 Introduction Atmosphere can be defined as mixture of gases or gaseous envelope that surrounds earth or any other planet or celestial here is held by the gravity of the body.

Earth’s atmosphere consists of oxygen which helps organisms for respiration. Earth’s atmosphere also consists of carbon. Earth’s temperature depends on how much sunlight the land, oceans, and atmosphere absorb, and how much heat the planet radiates back to space. This fact sheet describes the net flow of energy through different parts of the Earth system, and explains how the planetary energy budget stays in balance.

In the second half of the nineteenth century two prominent scientists, working in two distinct specialties, identified the importance of atmospheric trace constituents as efficient absorbers of long-wave radiation and as factors in climatic control.

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John Tyndall conducted the first convincing experiments on the radiative properties of gases, demonstrating that “perfectly colorless and. Earth’s relatively thin atmosphere primarily consists of a mixture of nitrogen (78%) and oxygen (21%) gases.

The remaining 1% contains several inactive gases (i.e., argon, neon, helium, hydrogen, and xenon) and several other gases that vary in concentration (i.e., water vapor, carbon dioxide, methane, nitrous oxide, ozone, and chlorofluorocarbons).

heat. atmosphere not only cools the Earth’s surfaces, it produces circulations in the atmosphere. These circulations are significantly different than those that result from the uneven heating of the Earth’s 3. When enough cloud droplets grow to precipitable surface by the Sun.

size, they fall to the Earth’s surface as rain/snow/ sleet, etc. Earth, like the other inner planets, receives virtually all of its energy from space in the form of solar electromagnetic radiation. Its total heat content does not vary significantly with time, indicating a close overall balance between absorbed solar radiation and the diffuse stream of low-temperature, thermal radiation emitted by the planet.

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The transformation of the incident solar. The solar radiation outside the earth's atmosphere is calculated using the radiant power density (H sun) at the sun's surface ( x 10 7 W/m 2), the radius of the sun (R sun), and the distance between the earth and the calculated solar irradiance at the Earth's atmosphere is about kW/m geometrical constants used in the calculation of the solar irradiance incident on the.

Gases in Earth's Atmosphere. Nitrogen and oxygen are by far the most common; dry air is composed of about 78% nitrogen (N 2) and about 21% oxygen (O 2).

Argon, carbon dioxide (CO 2), and many other gases are also present in much lower amounts; each makes up less than 1% of the atmosphere's mixture of gases. The atmosphere also includes water vapor. Sunlight drives the Earth’s weather, climate, chemistry, and biosphere. Recent efforts to improve solar heating codes in climate models focused on more accurate treatment of the absorption spectrum or fractional clouds.

A mostly forgotten assumption in climate models is that of a flat Earth atmosphere. Space-based solar power (SBSP) is the concept of collecting solar power in outer space and distributing it to ial advantages of collecting solar energy in space include a higher collection rate and a longer collection period due to the lack of a diffusing atmosphere, and the possibility of placing a solar collector in an orbiting location where there is no night.

beginning with the fact that more incoming solar radiation is absorbed by earths surface than by the atmosphere, describe the mechanism responsible for atmospheric heating most of the energy that is absorbed of earths surface is reradiated skyward in the form of infrared radiation.

Earth's atmosphere is made almost entirely oxygen (21 percent) and nitrogen (78 percent). Both gases are largely invisible to infrared radiation emitted by Earth.

Thermal energy. Among the most common devices used to capture solar energy and convert it to thermal energy are flat-plate collectors, which are used for solar heating applications.

Because the intensity of solar radiation at Earth’s surface is so low, these collectors must be large in area.

Even in sunny parts of the world’s temperate regions, for instance, a collector must have a surface. In this sense, Earth's atmosphere is sort of the "flip side" of the Sun's atmosphere.

The Greenhouse Effect Most of the solar radiation that reaches the Earth or its lower atmosphere, where albedo from clouds and features on the ground come into play, is thus in the form of visible light.heat (heat lamps for food in restaurants) (night vision goggles) what happens when sun/solar energy enters Earth's atmosphere.

most of it is absorbed in the mesosphere, then the rest is reflected and scattered all around the absorption and reflection of solar radiation help to balance Earth's .Heat Transfer in the Atmosphere. Heat moves in the atmosphere the same way it moves through the solid Earth (Plate Tectonics chapter) or another medium.

What follows is a review of the way heat flows, but applied to the atmosphere. Radiation is the transfer of energy between two objects by electromagnetic waves.