A Non-Equilibrium Model of Hemispheric Mean Surface Temperature

Bryson, Reid A.; Dittberner, Gerald J.

doi:10.1175/1520-0469(1976)033<2094:anemoh>2.0.co;2

Cited by 51 publications

(21 citation statements)

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“…It is then modulated by volcanic aerosol as it passes through the atmosphere (Goodman, 1984). Clouds were treated as done by Bryson and Dittberner (1976). The albedo variable was based in part on the isochrones at the edge of the ice sheet (Bryson et al, 1969) and the albedo of old and new ice and snow (Kung et al, 1964).…”

Section: Methodsmentioning

confidence: 99%

Changing growing conditions for crops during the Near Eastern Bronze Age (3000–1200 BC): the stable carbon isotope evidence

Riehl¹,

Bryson²,

Pustovoytov³

2008

Journal of Archaeological Science

103

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Section: Methodsmentioning

confidence: 99%

Changing growing conditions for crops during the Near Eastern Bronze Age (3000–1200 BC): the stable carbon isotope evidence

Riehl¹,

Bryson²,

Pustovoytov³

2008

Journal of Archaeological Science

103

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“…The anthropogenic hypothesis contends atmospheric transmission is changing, usually decreasing, on spatial scales up to hemispheric (e.g., Bryson and Dittberner, 1976)which then alters the global mean temperature. The Davos data alone would indicate global or hemispheric changes in atmospheric transmission are unlikely.…”

Section: Addendummentioning

confidence: 99%

Atmospheric transmission at Davos, Switzerland 1909?1979

Hoyt

Fröhlich

1990

Climatic Change

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Pyrheliometric measurements at Davos, Switzerland from 1909 to 1979 are used to reconstruct the time history of atmospheric transmission. Measurements were numerous enough to allow yearly and seasonal values of atmospheric transmission to be determined. Other than the eruptions of Katmal in 1912 and Agung in 1963, there are no significant long-term changes in atmospheric transmission observed at this central European site. The implications of this result upon those theories of climatic change which depend upon changes in atmospheric transmission are briefly considered.

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“…In the last two centuries the idea has also emerged that climatic variation in time the past century have been based on the assumption that the transparency of the cloudless atmosphere has varied-specifically, as related to this article, in response to variations of volcanically produced turbidity (2).…”

mentioning

confidence: 99%

Volcanic Activity and Climatic Changes

Bryson

Goodman

1980

Science

Self Cite

104

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Radiocarbon dates of volcanic activity suggest variations that appear to be related to climatic changes. Historical eruption records also show variations on the scale of years to centuries. These records can be combined with simple climatic models to estimate the impact of various volcanic activity levels. From this analysis it appears that climatic prediction in the range of 2 years to many decades requires broad-scale volcanic activity prediction. Statistical analysis of the volcanic record suggests that some predictability is possible.

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A Non-Equilibrium Model of Hemispheric Mean Surface Temperature

Cited by 51 publications

References 0 publications

Changing growing conditions for crops during the Near Eastern Bronze Age (3000–1200 BC): the stable carbon isotope evidence

Changing growing conditions for crops during the Near Eastern Bronze Age (3000–1200 BC): the stable carbon isotope evidence

Atmospheric transmission at Davos, Switzerland 1909?1979

Volcanic Activity and Climatic Changes

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