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1.
Summary The paper presents a review of the possibilities of using meteorological satellites for investigating various atmospheric phenomena and obtaining data on the physical condition of the atmosphere required for realizing the numerical methods of weather forecast, the synoptical analysis and other purposes. To avoid repetition the review does not include the much important material in the field of satellite meteorology which had been dealt with in earlier reviews.
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Elena D. Kireeva Olga B. Popovicheva Natalia M. Persiantseva Mikhail A. Timofeyev Natalia K. Shonija 《Journal of Atmospheric Chemistry》2009,64(2-3):129-147
Combustion-derived particles emitted by various transport engines are analyzed with respect to their morphology and composition. Soot particles collected behind an aircraft gas turbine engine combustor, in the diesel engine exhaust pipe, and at the end of ship pipe demonstrate heterogeneous morphological structures and different chemical identities. Individual particle analysis allows the characterization of emitted soot particles into three fractions, namely C-O, C-O-S, and Fe-C-O, with the dominant presence of chain soot agglomerates, irregular internally mixed soot, and particles of distinct morphology, respectively. The influence of oxygen and sulfur concentrations on the ability of soot to uptake water is proposed as a method for categorizing transport engine-generated particles. Categories of hydrophobic and hydrophilic particles within non-hygroscopic soots can be defined based on the amount of water uptake relative to several reference laboratory-made soots comparable to transport engine emissions. This method of characterizing hydrophobic/hydrophilic and hygroscopic soots in combustion emissions will help to determine the potential impacts of the combustion emissions on CCN/IN formation in the atmosphere. 相似文献
3.
Timofeyev Yu. M. Nerobelov G. M. Poberovskii A. V. Filippov N. N. 《Izvestiya Atmospheric and Oceanic Physics》2021,57(3):286-296
Izvestiya, Atmospheric and Oceanic Physics - Results obtained from ground-based high spectral resolution measurements of solar IR radiation absorption spectra are analyzed. These measurements have... 相似文献
4.
V. V. Asmus Yu. M. Timofeyev A. V. Polyakov A. B. Uspensky Yu. M. Golovin F. S. Zavelevich D. A. Kozlov A. N. Rublev A. V. Kukharsky V. P. Pyatkin E. V. Rusin 《Izvestiya Atmospheric and Oceanic Physics》2017,53(4):428-432
Preliminary results of a space experiment using the IKFS-2 infrared sounder (Meteor-M2 satellite) showed high-quality of measurements of spectra of the outgoing thermal radiation of the atmosphere–surface system and the adequacy of developed IR radiation atmospheric models in the 15-μm carbon gas absorption band used to recover the vertical profiles of the atmospheric temperature. Outgoing radiation spectra measured by IKFS-2 instruments make it possible to restore vertical temperature profiles with errors close to 1K in most of the 0–30 km high-altitude region, except for the lower troposphere and altitudes above 30 km, where these errors are close to 2–3K. 相似文献
5.
I.?A.?Berezin Yu.?M.?Timofeyev Ya.?A.?VirolainenEmail author I.?S.?Frantsuzova K.?A.?Volkova A.?V.?Poberovsky B.?N.?Holben A.?Smirnov I.?Slutsker 《Izvestiya Atmospheric and Oceanic Physics》2017,53(1):58-64
Water vapor plays a key role in weather and climate forming, which leads to the need for continuous monitoring of its content in different parts of the Earth. Intercomparison and validation of different methods for integrated water vapor (IWV) measurements are essential for determining the real accuracies of these methods. CIMEL photometers measure IWV at hundreds of ground-based stations of the AERONET network. We analyze simultaneous IWV measurements performed by a CIMEL photometer, an RPG-HATPRO MW radiometer, and a FTIR Bruker 125-HR spectrometer at the Peterhof station of St. Petersburg State University. We show that the CIMEL photometer calibrated by the manufacturer significantly underestimates the IWV obtained by other devices. We may conclude from this intercomparison that it is necessary to perform an additional calibration of the CIMEL photometer, as well as a possible correction of the interpretation technique for CIMEL measurements at the Peterhof site. 相似文献
6.
Spatial–Temporal CO2 Variations near St. Petersburg Based on Satellite and Ground-Based Measurements
Timofeyev Yu. M. Berezin I. A. Virolainen Ya. A. Makarova M. V. Polyakov A. V. Poberovsky A. V. Filippov N. N. Foka S. Ch. 《Izvestiya Atmospheric and Oceanic Physics》2019,55(1):59-64
Izvestiya, Atmospheric and Oceanic Physics - The results of studying spatial–temporal CO2 variations near St. Petersburg in 2014–2017 based on satellite measurements (OCO-2 satellite)... 相似文献
7.
A. M. Chayka Yu. M. Timofeyev A. V. Polyakov 《Izvestiya Atmospheric and Oceanic Physics》2008,44(2):193-206
The surface area and volume densities (S and V) of the particles of stratospheric background aerosol in the 15–20 km and 20–25 km layers for 2002–2005 were obtained from measurements of the aerosol extinction coefficient with the SAGE III instrument by using the linear-regression method of solving the inverse problem. The measurements were taken within the latitudinal belts 43°–80°N and 34°–58°S. The spatial and temporal dependences of S and V demonstrate homogeneous distribution fields in summer, whereas noticeable inhomogeneities are observed in winter and early spring. In all years of the measurements, an increase in the integral characteristics of stratospheric background aerosol was observed during the fall-to-winter transition period. Longitudinal variations in S and V can be both slight and significant (50–70%). Analysis of the interannual variability of the mean areas and volumes of aerosol particles shows that their minima (as a rule) were observed in 2002 and their maxima were observed in 2005. In most of the cases, no monotonic annual variations in the aerosol characteristics are noted. The dependence of the aerosol parameters on the phase of the quasi-biennial oscillations of zonal wind in the stratosphere is observed. The data obtained for 2002–2005 are, on the whole, in good agreement with the climatological data obtained for 1996–1999. 相似文献
8.
试论地貌圈概念、属性及其与其它地表圈层关系 总被引：1，自引：0，他引：1
地貌圈作为地表圈层中的一个与人类生存、发展直接发生关系的圈层。它具有三维形态、物质结构及其运动与演化的四大属性，并在全球充分连续的基本圈层。主要以亚洲与邻区海陆地貌为例，通过地貌圈大中地貌以内动力为主而微地貌以外动力为主的成因概念及其形态、物质、运动与演化四大属性的基本事实，论证地貌圈存在的客观性及其在全球的连续性。论文在探讨地貌圈运动特征时，首次用岩石圈构造分层的现代概念，解析了现代板块边缘及其毗邻广大地区GPS所测试的地壳运动速度，普遍慢于以热点为参考架而确定的板块运动速度。最后，论文以地貌圈与其它地表圈层互相关系的简表，及其与内外环境圈的物质流与能量流等示意图，来呼吁加强地貌圈的基础与应用研究，这对推动地球科学及其与人类生存和可持续发展具有重要意义。 相似文献
9.
Virolainen Ya. A. Polyakov A. V. Timofeyev Yu. M. 《Izvestiya Atmospheric and Oceanic Physics》2021,57(2):148-158
Izvestiya, Atmospheric and Oceanic Physics - Ozone anomalies that occur in the winter–spring period in the Northern Hemisphere have been increasingly observed in recent decades not only in... 相似文献
10.
Y. A. Virolainen Y. M. Timofeyev S. P. Smyshlyaev M. A. Motsakov O. Kirner 《Izvestiya Atmospheric and Oceanic Physics》2017,53(9):911-917
A comparison between the numerical simulation results of ozone fields with different experimental data makes it possible to estimate the quality of models for their further use in reliable forecasts of ozone layer evolution. We analyze time series of satellite (SBUV) measurements of the total ozone column (TOC) and the ozone partial columns in two atmospheric layers (0–25 and 25–60 km) and compare them with the results of numerical simulation in the chemistry transport model (CTM) for the low and middle atmosphere and the chemistry climate model EMAC. The daily and monthly average ozone values, short-term periods of ozone depletion, and long-term trends of ozone columns are considered; all data sets relate to St. Petersburg and the period between 2000 and 2014. The statistical parameters (means, standard deviations, variations, medians, asymmetry parameter, etc.) of the ozone time series are quite similar for all datasets. However, the EMAC model systematically underestimates the ozone columns in all layers considered. The corresponding differences between satellite measurements and EMAC numerical simulations are (5 ± 5)% and (7 ± 7)% and (1 ± 4)% for the ozone column in the 0–25 and 25–60 km layers, respectively. The correspondent differences between SBUV measurements and CTM results amount to (0 ± 7)%, (1 ± 9)%, and (–2 ± 8)%. Both models describe the sudden episodes of the ozone minimum well, but the EMAC accuracy is much higher than that of the CTM, which often underestimates the ozone minima. Assessments of the long-term linear trends show that they are close to zero for all datasets for the period under study. 相似文献