{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,10,25]],"date-time":"2026-10-25T13:23:33Z","timestamp":1792934613163,"version":"4.5.0"},"reference-count":38,"publisher":"Walter de Gruyter GmbH","issue":"2","license":[{"start":{"date-parts":[[2014,10,1]],"date-time":"2014-10-01T00:00:00Z","timestamp":1412121600000},"content-version":"unspecified","delay-in-days":0,"URL":"http:\/\/creativecommons.org\/licenses\/by-nc-nd\/3.0\/"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[2014,10,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n                  <jats:p>Temperature inversions represent complex phenomena, specific for depression forms of relief which introduce changes in vertical zoning (Ap\u0103v\u0103loae, Apostle, P\u00eervulescu, 1986 by stable air stratification (Erhan, 1981), because of their morphological features, this is due to the interdependence of general movement and characteristics of the active surface, being the cause of their production (Ap\u0103v\u0103loae, et. al., 1984, 1986, 1987). The generation of thermal inversions, their intensity and frequency is a consequence of altitude topography, morphology, fragmentation, orientation and degree of closure to external drives. (Ap\u0103v\u0103loae, Apostle, P\u00eervulescu, 1988). Thermal inversions represent complex phenomena, specific to depression landforms that introduce changes within the vertical zoning (Ap\u0103v\u0103loae, Apostol, P\u00eervulescu, 1986) by stable air stratification (Matveev, 1958, Erhan, 1981, Yinghui Liu, 2002) where vertical thermal gradient is negative (Matveev, 1958), due to their morphological features, also as a consequence of the interdependance of general circulation and characteristics of the active surface, the cause of their generation (Ap\u0103v\u0103loae, et. al., 1984, 1986, 1987).<\/jats:p>","DOI":"10.2478\/pesd-2014-0040","type":"journal-article","created":{"date-parts":[[2015,1,12]],"date-time":"2015-01-12T03:22:37Z","timestamp":1421032957000},"page":"267-284","source":"Crossref","is-referenced-by-count":9,"title":["Frequency of Thermal Inversions Between Siret and Prut Rivers in 2013"],"prefix":"10.1515","volume":"8","author":[{"given":"Pavel","family":"Ichim","sequence":"first","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Liviu","family":"Apostol","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Lucian","family":"Sf\u00eec\u0103","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Adriana-Lucia","family":"Kadhim-Abid","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Vasilic\u0103","family":"Istrate","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"374","reference":[{"key":"ref371","first-page":"33","article-title":"Thermal valley inversion impact on the dispersion of a passive pollutant in a complex mountainous area Volume Issues Pages","volume":"24","author":"Sandrine Anquetin","year":"1999","journal-title":"Atmospheric Environment October"},{"key":"ref301","first-page":"95","article-title":"Surface - 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