Further Comments on “The Effect of Tropospheric Temperature Lapse Rates on the Ascent Rates of Pilot Balloons”

Murray, David P.; Auer, August H.

doi:10.1175/1520-0450(1976)015<0904:fcoeot>2.0.co;2

J. Appl. Meteor.

1976

DOI: 10.1175/1520-0450(1976)015<0904:fcoeot>2.0.co;2

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Further Comments on “The Effect of Tropospheric Temperature Lapse Rates on the Ascent Rates of Pilot Balloons”

David P. Murray¹,

August H. Auer²

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1981

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Sea breezes along the Canterbury coast in the vicinity of Christchurch, New Zealand

Sturman

Tyson

1981

J. Climatol.

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Observations sre presented suggesting the significance of sea breezes in producing distinctive diurnal boundary layer oscillations over Christchurch. Sea breeze effects are shown to be an all-year phenomenon reaching their maxima in summer. The interaction of onshore wind components with south-westerly gradient winds (even under cloudy conditions) appears to produce a distinctive all-seasons diurnal rhythm in the gradient wind. The development of shallow north-easterlies blowing into an orographically-induced lee trough, preceding the onset of ground north-westerlies, is shown to produce a complicated system of onshore airtlow when combined with the sea breeze. Under such conditions it is argued that a sea breeze return current may be discerned.Canterbury sea breezes are an important feature of the local climate and correspond in many respects to classical sea breeze models. Notwithstanding, it is their site-specific characteristics that render them of particular interest.

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Sea breezes along the Canterbury coast in the vicinity of Christchurch, New Zealand

Sturman

Tyson

1981

J. Climatol.

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Further Comments on “The Effect of Tropospheric Temperature Lapse Rates on the Ascent Rates of Pilot Balloons”

Cited by 1 publication

References 0 publications

Sea breezes along the Canterbury coast in the vicinity of Christchurch, New Zealand

Sea breezes along the Canterbury coast in the vicinity of Christchurch, New Zealand

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