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      <source-app name="Horizon">Horizon</source-app>
      <rec-number>1</rec-number>
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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Telesca, L.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Shaban, A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Gascoin, S.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Darwich, T.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Drapeau, Laurent</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">El Hage, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Faour, G.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Characterization of the time dynamics of monthly satellite snow cover data on Mountain Chains in Lebanon</title>
        <secondary-title>Journal of Hydrology</secondary-title>
      </titles>
      <pages>3214-3222</pages>
      <keywords>
        <keyword>Snowpack</keyword>
        <keyword>Satellite image</keyword>
        <keyword>SSA</keyword>
        <keyword>Periodogram</keyword>
        <keyword>Lebanon</keyword>
        <keyword>LIBAN</keyword>
      </keywords>
      <dates>
        <year>2014</year>
      </dates>
      <call-num>fdi:010063690</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Journal of Hydrology</full-title>
      </periodical>
      <isbn>0022-1694</isbn>
      <accession-num>ISI:000347589600041</accession-num>
      <number>D</number>
      <electronic-resource-num>10.1016/j.jhydrol.2014.10.037</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010063690</url>
        </related-urls>
        <pdf-urls>
          <url>https://www.documentation.ird.fr/intranet/publi/2015/02/010063690.pdf</url>
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      </urls>
      <volume>519</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>In this study, the time dynamics of the monthly means of the snow cover have been on Lebanese Mountain Chains from 2000 to 2012, derived from the MODIS Aqua/Terra satellite snow products was analyzed. This represents the longest satellite-based snow cover time series produced for Lebanon so far. Field survey was also carried out over the last three years in order to measure the in-situ snow/water equivalent and depth in different localities. Analyzing the regime of the snow cover in Mount-Lebanon (Western Mountain Chains) region, it was found that: (i) snowmelt accounts for about 31% of the rivers and springs discharge in Lebanon; (ii) consecutive peaks in the snow cover time series, representing the change-point between accumulation phase and ablation phase are present in three different patterns (edged, non-edged and double peaked); (iii) the areal snow coverage has big diversity between different years; (iv) the annual periodicity represents the most statistically significant and predominant frequency of the series contributing for about the 40% of the total variance of the snow cover series; (v) the longterm trend, totally hidden by the more powerful yearly component and detected by using the singular spectrum analysis (SSA), accounts for about the 33% of the total variance of the series; (vi) the long-term trend shows an apparent cyclic behavior with an estimated period (interval between the two minima) of about nine years; (vii) the comparison of the long-term trend with the North Atlantic Oscillation (NAO) monthly index reveals that the minima in 2009-2010 of the SSA long-term component coincides with a persistent negative phase in the NAO Index.</abstract>
      <custom6>062 ; 126</custom6>
      <custom1>UR113</custom1>
      <custom7>Liban</custom7>
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