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Vol 41, No 1 (2016)

Article

Winter climatology of upper-level frontal zones in the Northern Hemisphere

Razorenova O.A.

Abstract

Average long-term fields of geopotential gradients in the middle and upper troposphere and temperature gradients and geopotential Laplacian in the middle troposphere in the Northern Hemisphere in winter are analyzed. Based on the analysis of the distribution of the maximum values of gradients, the average long-term position of upper-level frontal zones and their axial lines was determined. Their spatial distribution is analyzed from the point of view of interaction between thermobaric fields over different regions of the globe. Average long-term parameters of upper-level frontal zones in the middle troposphere are presented. Average long-term fields of wind speed in the middle and upper troposphere are investigated. It is demonstrated that the zones of the maximum values of wind speed agree well with the position of separated upper-level frontal zones.

Russian Meteorology and Hydrology. 2016;41(1):1-9
pages 1-9 views

Estimating the trends and variability of atmospheric action centers over the Asian-Pacific region in summer in 1950–1979 and 1980–2012

Shatilina T.A., Tsitsiashvili G.S., Radchenkova T.V.

Abstract

The trend significance and the residual variability of integral atmospheric characteristics in the atmospheric action centers in the Asian-Pacific region in summer in 1950-1979 and 1980-2012 are computed. Basic differences are revealed between trends in circulation and residual variability in the atmo spheric action centers in the surface pressure field and in the field of geopotential H500 for these time periods. Increase in significant trends for the whole period and decrease in residual variability were found in the area of the Asian low in 1980-2012. A significant trend was observed in June and September in the area of the Hawaiian high. The summer Far Eastern low has intensified in recent years. The Okhotsk high strengthened in May and weakened in June, August, and September in the 2000s.

Russian Meteorology and Hydrology. 2016;41(1):10-18
pages 10-18 views

Physiographic factors of seasonal distribution of linear trends in air temperature on the Azov-Black sea coast

Evstigneev V.P., Naumova V.A., Evstigneev M.P., Lemeshko N.A.

Abstract

The seasonal distribution of linear trends in air temperature on the coast of the Black and Azov seas in 1936-2010 is analyzed using the quantile regression method. Monthly mean and median values of temperature as well as 10% and 90% quantiles of average daily values of temperature are considered to describe changes in extreme positive and negative temperature anomalies. It is demonstrated that besides tendencies that are common for all meteorological stations, local features and physiographic location of the stations are of great importance for the distribution of temperature trends.

Russian Meteorology and Hydrology. 2016;41(1):19-27
pages 19-27 views

Satellite-derived peculiarities of total ozone field under atmospheric blocking conditions over the European part of Russia in summer 2010

Sitnov S.A., Mokhov I.I.

Abstract

Based on the AIRS satellite spectrometer data (the Aqua platform), the peculiarities are studied of the field of total ozone (TO) under prolonged blocking conditions over the European part of Russia in summer 2010. It is revealed that the spatial distribution of TO values during the period of blocking was characterized by negative TO anomalies (up to -37 DU on the first ten days of August) over the western and northern peripheries of the blocking anticyclone and by positive TO anomalies (up to 60 DU) over the troughs adj oinmg the anticyclone. Possible mechanisms of the formation of TO anomalies are discussed. The results are presented of the validation of TO measurements with the AIRS spectrometer in May-September 2010 obtained from the data of TO measurements with Brewer spectrophotometers at Kislovodsk and Obninsk stations of the global ozone network.

Russian Meteorology and Hydrology. 2016;41(1):28-36
pages 28-36 views

Methane emission from West Siberian forest-steppe and subtaiga reed fens

Sabrekov A.F., Filippov I.V., Glagolev M.V., Terent’eva I.E., Il’yasov D.V., Kotsyurbenko O.R., Maksyutov S.S.

Abstract

Methane emission from West Siberian forest-steppe and subtaiga reed fens (that is, fens dominated by Phragmites australis) observed in summer 2013, is considered using the static chamber method. The obtained medians of CH4 fluxes varied from -0.08 to 2.7 mg CH4/m2 per hour. Eenvironmental factors affecting methane emission are analyzed. It was found that CH4 emissions from the reed fens correlate only with the concentration of salt ions in the wetland water and with the plant community structure. The latter probably also depends on water salinity. It was revealed that in fens the ratio between fluxes of CH4 and CO2 does not depend on the water table level that contradicts the general pattern simulated by mathematical models of CH4 emission. It was found that Phragmites australis fens and similar ecosystems should be considered as a separate wetland class from the point of view of methane emission study.

Russian Meteorology and Hydrology. 2016;41(1):37-42
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Spatiotemporal variability of the flow in the deep part of the Central Caspian Sea

Ambrosimov A.K.

Abstract

The paper presents the analysis of hydrophysical observations executed along the Transcaspian section in 2004-2014 during the expeditions by Shirshov Institute of Oceanology of Russian Academy of Sciences. The results used in the paper are the generalization of data obtained in the last decade. Investigations of the current system of the Central Caspian Sea demonstrated that at the northeastern part of the cyclonic circulation there are considerable deviations. The deposits that energy of current disturbances of various spatiotemporal scales makes to the general energy of currents, are calculated. Preliminary results are received of the assessment of water transfer through the Apsheron threshold from the Central to the Southern Caspian Sea and vice versa. It is shown that annual recurrence of concentration of hydrogen sulfide in the benthonic hollows of the Caspian Sea is directly connected with seasonal and synoptic variability of currents at the bottom.

Russian Meteorology and Hydrology. 2016;41(1):43-56
pages 43-56 views

Seiche oscillations in the Nakhodka Gulf

Smirnov S.V.

Abstract

Spatiotemporal parameters of barotropic seiche oscillations in the Nakhodka Gulf in the Sea of Japan are considered using the spectral finite-difference model. The finite-difference approximation of shallow water equations is carried out at the irregular triangular spatial grid. The sets of periods and spatial structures of seiche oscillations corresponding to the strongly pronounced maxima of energy spectrum of sea level data from Nakhodka station of the Russian tsunami warning service are computed and presented.

Russian Meteorology and Hydrology. 2016;41(1):57-62
pages 57-62 views

Potential of river network modeling based on GIS technologies and digital elevation model

Gartsman B.I., Shekman E.A.

Abstract

The development of GIS technologies and the availability of a wide range of geodatasets provide great potential for modeling physiographic objects, in particular, river systems. The adequate automatic method of river network digitizing was developed and tested using the digital elevation model based on applying the Complex Energy Index (CEI); the results are presented. The index form includes the independent parameterization of main geomorphologic and climatic factors of the first-order stream generation. The method testing proved that it is efficient and the results of its use can be reliably interpreted. The software was developed on the basis of ArcGIS tools. It implements the full algorithm of the automatic digitizing of river network using the digital elevation model. It also allows advancing studies on this issue, and could be used for solving applied problems.

Russian Meteorology and Hydrology. 2016;41(1):63-71
pages 63-71 views

On the problem of velocity of long continuous waves in overland flows

Natishvili O.G.

Abstract

The velocity of one-dimensional long continuous wave is computed from the condition of continuity of water both with its variable and constant discharge along the way passing through the control volume of water moving with the velocity VW. The wave stability on the free surface of an overland flow is analyzed.

Russian Meteorology and Hydrology. 2016;41(1):72-75
pages 72-75 views