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SMPS Spectra during Various Meteorological Conditions

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F11%3A10110280" target="_blank" >RIV/00216208:11320/11:10110280 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985858:_____/11:00366473

  • Result on the web

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    čeština

  • Original language name

    SMPS spektra při různých meteorologických podmínkách

  • Original language description

    Particle size distributions (PSD) of atmospheric aerosols have been studied extensively due to the confirmed influence of aerosols on global climate, aerosol - clouds interactions, atmospheric visibility, human health etc. (Kerminen et al 2005; IPCC, 2007; Wichmann et al, 2000). Strong feedback mechanisms of the atmosphere acting on PSD have been found as well Mikkonen et al, 2011). To evaluate these feedbacks, it is necessary to describe a connection between individual meteorological phenomena and atmospheric aerosol. The variety of measured meteorological variables able to alter or adapt aerosol PSD in its shape or amplitude is wide. Their contributions vary a lot, however. The most important characteristics, besides temperature, radiation and wind speed, are relative humidity (RH) and precipitation amount (Zíková et al, 2010). This work describes first results of categorization of aerosol PSD according to the various meteorological conditions connected to atmospheric humidity.

  • Czech name

    SMPS spektra při různých meteorologických podmínkách

  • Czech description

    Particle size distributions (PSD) of atmospheric aerosols have been studied extensively due to the confirmed influence of aerosols on global climate, aerosol - clouds interactions, atmospheric visibility, human health etc. (Kerminen et al 2005; IPCC, 2007; Wichmann et al, 2000). Strong feedback mechanisms of the atmosphere acting on PSD have been found as well Mikkonen et al, 2011). To evaluate these feedbacks, it is necessary to describe a connection between individual meteorological phenomena and atmospheric aerosol. The variety of measured meteorological variables able to alter or adapt aerosol PSD in its shape or amplitude is wide. Their contributions vary a lot, however. The most important characteristics, besides temperature, radiation and wind speed, are relative humidity (RH) and precipitation amount (Zíková et al, 2010). This work describes first results of categorization of aerosol PSD according to the various meteorological conditions connected to atmospheric humidity.

Classification

  • Type

    D - Article in proceedings

  • CEP classification

    DG - Atmospheric sciences, meteorology

  • OECD FORD branch

Result continuities

  • Project

  • Continuities

    Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2011

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Article name in the collection

    PROCEEDINGS OF 12TH ANNUAL CONFERENCE OF THE CZECH AEROSOL SOCIETY

  • ISBN

    978-80-86186-31-3

  • ISSN

  • e-ISSN

  • Number of pages

    4

  • Pages from-to

    75-78

  • Publisher name

    Česká aerosolová společnost

  • Place of publication

    Praha

  • Event location

    Čejkovice

  • Event date

    Nov 3, 2011

  • Type of event by nationality

    EUR - Evropská akce

  • UT code for WoS article