The city of Athens, especially in summer, comes under the influence of sea breeze and the Etesian winds, some characteristic elements of which are given for the period 1921–1930. The diurnal march of July dew point at Athens is clearly double with main extremes at the afternoon and the secondaries in the forenoon time. However, on days with uninterrupted sea breeze three pairs of extremes characterize the variation, there being two secondary maxima and two secondary minima in the forenoon. On days, on the other hand, with uninterrupted Etesian winds the appearing double diurnal march is characterized by the forenoon main maximum and the afternoon main minimum.
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Photios P. Karapiperis,Characteristics of local winds at Athens, Greece, Geof. pura e appl.25 (1953), 203.
Leon. N. Carapiperis,Symvoli es ten meleten ton epidraseon ton Etesion kai tes thalassias auras epi tes thermokrasias kai hygrasias aeros Athenon (Contribution à l'étude de l'influence des ètésiens et de la brise de mer sur la température et l'humidité de l'air d'Athènes), Praktika tes Academias Athenon29 (1954), 420.
Photios P. Karapiperis,Symvoli es ten meleten tes hemereseas poreas tes apolytou hygtasias en Athenais (Contribution to the study of diurnal march of absolute humidity at Athens), Hypomnemata tou Ethnikou Asteroskopeou Athenon, Sera II, Meteorol.8 (1962).
O. G. Sutton,Micrometeorology, 1953, 5.
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Karapiperis, P.P. The influence of sea breeze and Etesian winds on the diurnal march of dew point at Athens, Greece. PAGEOPH 58, 221–224 (1964). https://doi.org/10.1007/BF00879150
- Characteristic Element
- Secondary Maximum
- Main Maximum
- Secondary Minimum
- Etesian Wind