Last edited by Mazuru
Tuesday, July 14, 2020 | History

2 edition of Atmospheric turbidity over Jerusalem. found in the catalog.

Atmospheric turbidity over Jerusalem.

Alexander Manes

Atmospheric turbidity over Jerusalem.

by Alexander Manes

  • 43 Want to read
  • 36 Currently reading

Published by Israel Meteorological Service, Research and Development Division in Bet-Dagan .
Written in English

    Places:
  • Jerusalem.
    • Subjects:
    • Atmospheric turbidity -- Jerusalem.

    • Edition Notes

      SeriesIsrael Meteorological Service. Series A, Meteorological notes, no. 26, Sidrah A--Reshimot meṭeʼorologiyot ;, mis. 26.
      Classifications
      LC ClassificationsQC990.P3 A35 no. 26, QC976.T8 A35 no. 26
      The Physical Object
      Pagination81 l.
      Number of Pages81
      ID Numbers
      Open LibraryOL5081258M
      LC Control Number74152257

        Books. Publishing Support. Login. Placed in a narrow path between two mountain chains that direct and accelerate the surface winds over the depression, the Bodélé emits dust on 40% of the winter days, averaging more than million tons of dust per day. Carlson T N Atmospheric turbidity in Saharan dust outbreaks as determined by. Ruth Ward Heflin has 14 books on Goodreads with ratings. Ruth Ward Heflin’s most popular book is Glory: Experiencing the Atmosphere of g: turbidity.

        Jerusalem: Chronicles from the Holy City is the product of a year-long stay in the region and, over the course of more than pages, tries to make Author: Ben Lerwill. Jerusalem Weather Station Height m Tue 28/04/ Share. About. Back; feels like Atmospheric pressure is the pressure above any area in the Earth's atmosphere caused by the weight of air on a square unit of the earth.

      Its value depends on the composition of the air, i.e., on its humidity. For average atmospheric conditions a value c p = MJ kg-1 °C-1 can be used. As an average atmospheric pressure is used for each location (Equation 7), the psychrometric constant is kept constant for each g: Jerusalem. Extraordinarily high atmospheric turbidity was observed in Estonia in and in , resulting from the eruptions of El Chichón () and Mount Pinatubo (). Then the annual mean flux densities of direct solar radiation were 82 and 78% of the average over –, by:


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Atmospheric turbidity over Jerusalem by Alexander Manes Download PDF EPUB FB2

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Buy Atmospheric turbidity over Jerusalem (Israel Meteorological Service. Series A, Meteorological notes, no. 26) by Alexander Manes (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Alexander Manes. Seasonal and synoptic variations in the optical depth of the atmospheric aerosol and in its wavelength dependence in the visible part of the spectrum are given and compared with those at other locations.

A secular increase in the turbidity of about 10% per decade, sincecould be isolated in this by: One of the more obvious indications of atmospheric pollution is the presence of solid or liquid particles, called aerosols, dispersed in the air. Global Environmental Issues book. A Climatological Approach.

Global Environmental Issues. Atmospheric turbidity Missing: Jerusalem. Abstract. On the basis of the scale of the phenomenon being monitored, air pollution monitoring problems can be divided into two general categories: 1) local monitoring and 2) regional and global : George Ohring, Joseph Otterman, Joachim Joseph.

Buy Atmospheric Turbidity over the United States from by U.S. Environmental Protection Agency (ISBN: ) from Amazon's Book Store. Everyday low Format: Paperback. Estimation of the Linke and Unsworth-Monteith turbidity factors in the visible spectrum: Application for Athens, Greece Manes A.

() Atmospheric turbidity over Jerusalem. Abstract. In three strong dust episodes occurred in the Eastern Mediterranean Basin during the rainy season September and October. During dust episodes, and at normal conditions in order to compare dust and non-dust period, daily PM aerosol samples and weekly six stage size separated aerosol samples were collected at Antalya, an eastern Mediterranean by: 9.

Atmospheric Environ- erally monotonic composition and are enriched in Ca m compared to accepted values for Saharan and world Joseph J. and Manes A. () Secular and seasonal aerosols. The samples were also enriched in Pb due to variation of atmospheric turbidity over Jerusalem.

appl. Met. 10, traffic by: Estimation of atmospheric turbidity over Ghardaïa city Djelloul Djafer, Abdanour Irbah To cite this version: Djelloul Djafer, Abdanour Irbah. Estimation of atmospheric turbidity over Ghardaïa city. Atmo-spheric Research, Elsevier, pp ￿/es￿.

￿hal. Request PDF | On Jan 1,M. Tadros and others published Atmospheric Turbidity Parameters Affecting the Incident Solar Radiation For Two Different Areas in Egypt |. The computations were performed for the summer months over Jerusalem (°N; °E).

A standard ozone profile was used for a total ozone value of DU. In general, the results are given as hourly fluxes around noon; on the average the solar zenith angle at this period is 10–12°.Cited by: Atmospheric Turbidity over West-Africa D.

Henning and H. Flohn Some Aspects of Evaporation and Sensible Heat Flux of the Tropical Atlantic P. Koepke Calibration of the METEOSAT IR-Channel by Ground Measurements Book Reviews / Concise Book Reviews Contents 4/ W.G.

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K t turbidity coefficient [], 0 atmospheric pressure [kPa] f angle of the sun above the horizon [rad] W precipitable water in the atmosphere [mm] W = e a P + () where: W precipitable water in the atmosphere [mm] e a actual vapour Missing: Jerusalem.

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