Current changes of the lower troposphere temperature in the Moscow region View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2017-07

AUTHORS

M. A. Lokoshchenko, I. A. Korneva, A. V. Kochin, A. Z. Dubovetsky, M. A. Novitsky, P. Ye. Razin

ABSTRACT

Modern climatic changes for 1991–2013 in the lower 4-km layer of the atmosphere in the Moscow region are discussed based on long-term measurements using radiosondes in Dolgoprudny near Moscow and sensors installed on a high mast in Obninsk and on a television tower in Ostankino in Moscow. It is shown that at the end of the 20th century and the beginning of the 21st century the mean-annual air temperature at all heights from 2 to 4000 m increased by an average of 0.1°C per year. In recent years, the warming has slowed. Over the last two decades, long-term changes were multidirectional, depending on the season: warming in May–December, cooling in January–February, and no statistically significant changes in March and April. The probable reason for the temperature decrease in the middle of the cold period is changes in the large-scale atmospheric circulation during recent years (the negative phase of the North Atlantic Oscillation in early 2010s). In recent years, the Moscow region climate continentality has increased because of warming in summer and cooling in winter, despite the secular decreasing trend, which was noted before. Mean daily and annual warming rates in Dolgoprudny were higher than in Obninsk. The probable reason is the northward construction expansion and the strengthening of the Moscow heat island. The highest annual temperature amplitude is recorded at heights of 200–300 m. More... »

PAGES

392-401

References to SciGraph publications

  • 2016-05. Air temperature in the lower troposphere over moscow during heat wave in the summer of 2010 in ATMOSPHERIC AND OCEANIC OPTICS
  • 2012-09. Catastrophic heat of 2010 in Moscow from data of ground-based meteorological measurements in IZVESTIYA, ATMOSPHERIC AND OCEANIC PHYSICS
  • 2015-09. On the problem of the global climate change in RUSSIAN METEOROLOGY AND HYDROLOGY
  • 2007-01. Temperature stratification of the lower atmosphere over Moscow in RUSSIAN METEOROLOGY AND HYDROLOGY
  • 2008-01. Causes of November cooling of the 1980s–1990s in European Russia in RUSSIAN METEOROLOGY AND HYDROLOGY
  • 2016-01. Vertical extension of the urban heat island above Moscow in DOKLADY EARTH SCIENCES
  • Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1134/s0001433817040089

    DOI

    http://dx.doi.org/10.1134/s0001433817040089

    DIMENSIONS

    https://app.dimensions.ai/details/publication/pub.1091309137


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