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Том 41, № 3 (2016)

Article

GIS-Amur system of flood monitoring, forecasting, and early warning

Frolov A., Asmus V., Borshch S., Vil’fand R., Zhabina I., Zatyagalova V., Krovotyntsev V., Kudryavtseva O., Leont’eva E., Simonov Y., Stepanov Y.

Аннотация

GIS-Amur system offlood monitoring, forecasting, and early warning was developed at the Hydrometcenter of Russia and Planeta Research Center for Space Hydrometeorology for the effective surveill ance of hydrological conditions in the Amur River basin. The system is based on the use of hydrometeorological information, that is, observational data from weather and gaging stations, data from hydrological forecasts, and satellite data. The GIS- and web-based GIS-Amur system provides high reliability, safety, and operational speed. During the operational practice in the spring and summer 2015, the system demonstrated the forecast accuracy and reliability, the timely delivery of output products to end users, and the great variety of the output product types and formats. The system provides near-real time access to all available hydrometeorological data in the Amur River basin that favors correct and timely decision-making for flood risk reduction.

Russian Meteorology and Hydrology. 2016;41(3):157-169
pages 157-169 views

Stratosphere-troposphere exchange and its specific features at extratropical latitudes

Ivanova A.

Аннотация

A review of the papers dealing with various aspects of stratosphere-troposphere exchange (STE) is presented. The development of STE concepts is described and quantitative estimates of STE obtained by different authors are given. Typical time scales and geographic features of STE are described. Special attention is given to the specific features of STE at extratropical latitudes where active vertical air transport is observed in both directions. The air ascent through the tropopause occurs there in the zones of warm conveyor belts, and the air descent takes place in the zones of stratospheric intrusions. Exchange processes in the key region including the upper troposphere and the lowermost stratosphere are described. The mechanisms of large-scale stratospheric intrusions in the systems of tropopause folds or cut-off lows are presented as well as the mechanisms of the mixing of the stratospheric air with the tropospheric one. Specific features of deep stratospheric intrusions are discussed which are based on the analysis of such indicators of stratospheric air as high concentrations of ozone and stratospheric radionuclide 7Be. Some aspects of stratosphere-troposphere energy exchange are considered.

Russian Meteorology and Hydrology. 2016;41(3):170-185
pages 170-185 views

Atmospheric electric field strength and thunderstorms in the North Caucasus

Adzhiev A., Stasenko V., Shapovalov A., Shapovalov V.

Аннотация

The results ofthe joint analysis ofthe data ofinstrumental observations using LS8000 lightning detector, weather radars (MRL-5 and DMRL-C), and electric field strength sensors as well as the results of numerical simulation of electric parameters of developed convective clouds based on the three-dimensional model worked out at High-mountain Geophysical Institute are presented. Some results of mathematical modeling of electric charges and fields in a convective cloud in the process of its evolution are described. The computations are based on the real data of atmospheric upper-air sounding on the days with thunderstorm and hailstorm processes in the North Caucasus. The effects of electric processes on the formation of micro structural parameters of convective clouds and precipitation are studied.

Russian Meteorology and Hydrology. 2016;41(3):186-192
pages 186-192 views

Estimating the accuracy of the very heavy snowfall forecast in the Urals by the WRF model

Kalinin N., Vetrov A., Pishchal’nikova E., Sviyazov E., Shikhov A.

Аннотация

The results of the forecast of two heavy snowfalls registered on October 18 and 23, 2014 in the Urals using the WRF model are presented. The application of the WRF-ARW atmospheric model to the computation of weather forecasts for the conditions of heavy widespread precipitation in the form of snow is considered. The obtained estimates of precipitation forecast are compared with the estimates of the GFS NCEP global model. The results demonstrate that both models have approximately the same accuracy of precipitation forecast in the context of the process under consideration.

Russian Meteorology and Hydrology. 2016;41(3):193-198
pages 193-198 views

Methane concentration in the atmospheric boundary layer from the measurements at north pole-36 and north pole-39 drifting ice stations

Nagurnyi A., Makshtas A.

Аннотация

Episodic emissions ofmethane with the concentration of4 ppm to the lower atmosphere near the continental slope of the Arctic Ocean are considered. It is revealed that such methane emissions can be associated with the erosion of sediments containing gas hydrates, for example, as a result of the effects of mudflows caused by the instability of slope currents as well as by the geologic activity in the zone of significant depth drops. The high background concentration of methane is registered in the central part of the Arctic Ocean that is probably provoked by biologic activity within sea ice and on its bottom.

Russian Meteorology and Hydrology. 2016;41(3):199-204
pages 199-204 views

Distribution of methane content and methane fluxes in the Sea of Japan, Sea of Okhotsk, and near-Kuril Pacific

Obzhirov A., Pestrikova N., Mishukova G., Mishukov V., Okulov A.

Аннотация

The spatial distribution of methane content and methane fluxes in the water in the north-western part of the Sea of Japan, in the Kuril basin of the Sea of Okhotsk, and in the near-Kuril part of the Pacific Ocean is studied using the data of marine research expeditions in 2005, 2010, and 2011. The studies revealed the significant variability of the methane flux depending on the source presence and on the sea surface conditions. The high emission of methane from water to the atmosphere is registered in the areas where its concentration exceeds the equilibrium values with the atmosphere. The use of the model of computation of the fields of currents and contaminant transport for the investigated water area enabled explaining the formation of the high concentration of methane in the center of vortices in the zones of sea water convergence in the water areas under study.

Russian Meteorology and Hydrology. 2016;41(3):205-212
pages 205-212 views

Assessment of possible expansion of the climatic range of Italian locust (Calliptamus italicus L.) in Russia in the 21st century at simulated climate changes

Popova E., Semenov S., Popov I.

Аннотация

The areas of distribution, high pest damage, and mass reproduction of Italian locust are mainly limited by climatic factors. It is demonstrated that under conditions of the RCP4.5 moderate scenario of anthropogenic impact on the global climate system in Russia in the 21st century the climatic range of Italian locust will be expanded mainly northward and, to a smaller extent, eastward. The expansion of the range by the middle of the 21st century as compared with the end of the 20th century will be more significant that at the end of the 21st century versus its middle.

Russian Meteorology and Hydrology. 2016;41(3):213-217
pages 213-217 views

Communications

Soil moisture content in the Bryansk oblast under climate change

Selyutin V.

Аннотация

Quantitative estimates are obtained of long-term variations in moisture content in the active layer of soil on the territory of the Bryansk oblast.

Russian Meteorology and Hydrology. 2016;41(3):218-220
pages 218-220 views

Instruments, Observations, and Processing

Principles of quality control of upper-air sounding datasets

Aldukhov O., Chernykh I.

Аннотация

Basic principles of the quality control of aerological data are formulated. These principles are assumed as a basis for the procedure of the control of archival and current data of upper-air sounding at All-Russian Research Institute of Hydrometeorological Information-World Data Center including the section of aerological information of the Russian State Fund. It is demonstrated that the only possible way to solve a problem of creation of historical high-resolution global datasets is the use of the method of complex (multicomponent) quality control.

Russian Meteorology and Hydrology. 2016;41(3):221-227
pages 221-227 views

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