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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
361

Some development of a zonally averaged climate model

Shine, Keith Peter January 1981 (has links)
No description available.
362

Radiation and aerosol in the convective boundary layer

Warren, David Edward January 1983 (has links)
No description available.
363

Linear and nonlinear responses of a model atmosphere to large scale topography and diabatic heating

Lei, Zhao-Chong January 1986 (has links)
No description available.
364

Diabatic circulations in the stratosphere

Pawson, Steven January 1988 (has links)
No description available.
365

Stratospheric residual circulation as deduced from satellite data

Beagley, Stephen Reuben January 1989 (has links)
No description available.
366

Balance and potential vorticity inversion in atmospheric dynamics

Norton, Warwick Alexander January 1988 (has links)
No description available.
367

The mechanism of the oxygen airglow

Stott, Ian Peter January 1987 (has links)
It is well known that the atmosphere of the earth emits a glow throughout the night. The major contribution to this nightglow was first observed in 1901 and was later shown to be due to the transition: O(<SUP>1</SUP>S) → O(^1D) +<i>hv</i>. After many years of controversy, the accepted method for the production of the O(^1S) at a height around 100 km is the Barth mechanism: O(<SUP>3P) + O(<SUP>3P) + M →O <SUP>ast<SUB>2 + M </SUB></SUP>O<SUP>ast<SUB>2 + O(<SUP>3P) →O<SUB>2 + O(<SUP>1S)</SUB></SUP> Where O^ast_2 represents an excited species of oxygen. The precursor can be any of four possible states: O_2(<i>A</i>^3 Σ+_u), O_2(<i>c</i>^1Σ-_u), O_2(<i>A'</i>^3Δu) and O_2(^5πg). All of these states have been proposed as the O(^1S) precursor at one time or another, but none conclusively. For a long time it has been realised that atmospheric measurements of O(^1S), its possible precursors and other relevant species, needs to be taken simultaneously. However up to now this has not been achieved in the laboratory. In the work described here, O(^1S) and the three precursors O_2(<i>A</i>^3Σ+_u), O_2(<i>A'</i>^3Δu) and O_2(<i>c</i>^1Σ-_u) were observed in a laboratory fast flow system. A new method is described whereby upon the addition of a quencher to the system each species can be tested to see if it could be acting as the Barth precursor to O(^1S). Three different quenchers were added in turn; CO_2, SF_6 and O_2. The results gained lead to the conclusion that O_2(<i>c</i>^1Σ-_u), O_2(<i>A'</i>^3Δu) and O_2(<i>A</i>^3Σ+_u)(vleq4) cannot be acting as a O(^1S) precursor, and that O_2(<i>A</i>^3Σ+_u)(vgeq5) is able to do so. The absolute concentrations of O_2(A^3Σ+_u), O(^1S) and O(^3P) were measured and the results compared with the values of these quantities found at a height of 97 km in the earths atmosphere. This comparison shows that O_2(<i>A</i>^3Σ+_u)(vgeq5) can account for all the O(^1S) production at that height at night. The thesis concludes with a discussion of the application of the same method to the determination of the precursors for some of the excited species of O_2.
368

Internal variability of the middle atmosphere

Clark, Paul Duncan January 1992 (has links)
No description available.
369

Spectroscopic and kinetic studies of atmospherically important processes

Harwood, Matthew Henry January 1995 (has links)
No description available.
370

Measurement of stratospheric composition using ultraviolet and visible spectroscopy

Fish, Deborah Jane January 1995 (has links)
No description available.

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