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Carpathian Journal of Earth and Environmental Sciences

An International Peer-Reviewed Open Access Journal

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ARTICLE IN » Volume 6, 2011 - Number 1

THE CLIMATIC-TOURISTIC POTENTIAL OF THE ROMANIAN BLACK SEA COAST DURING SUMMER, ESTABLISHED ACCORDING TO THE METHOD OF BESANCENOT, MOUNIER AND DE LAVENNE



Liviu APOSTOL1 & Ovidiu GACEU2
1„Al. I. Cuza ” University, Iaşi, Department of Geography and Geology, B-dul Carol I nr. 20 A, Iaşi, Romania, tel/fax: 0040223974, e-mail: apostolliv@yahoo.com.
2University of Oradea, Department of Geography, Tourism and Territorial Development, str. Universităţii, nr. 1, cod 410087, Oradea, Romania, tel/fax: 00.40.259.408472, e-mail: gaceu@yahoo.com.

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Abstract

This paper describes the climatic-touristic potential of the Romanian Black Sea Coast during summer, based on daily weather data collected between 1960 and 2009 from the weather stations of Sf. Gheorghe, Gura Portiţei, Constanţa and Mangalia. These data have been processed using the method of Besancenot et al. (1978), establishing a classification which highlights the optimal combination of climatic elements influencing touristic outdoor activities. Following the analysis, we have concluded that the climatic-touristic potential of the Romanian Black Sea Coast is high, at it peak during July and August when very nice and sunny weather reaches a frequency of up to 61%. The less favorable month is September, the registered frequency of unfavorable weather during the first 20 years reaching 18-36% and 34-55% during the third decade.
Keywords:
  • climatic-touristic
  • potential
  • the
  • Black
  • Sea
  • method.

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© 2011 by the author(s). Licensee CJEES, Carpathian Association of Environment and Earth Sciences. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).

How to cite

Liviu APOSTOL & Ovidiu GACEU (2011). THE CLIMATIC-TOURISTIC POTENTIAL OF THE ROMANIAN BLACK SEA COAST DURING SUMMER, ESTABLISHED ACCORDING TO THE METHOD OF BESANCENOT, MOUNIER AND DE LAVENNE

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