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1.
By using the NCEP/NCAR reanalysis data sets for 1951–2001, we study the characteristics of Pacific cyclones. It is shown that the northeast-southwest
direction is predominant in the displacements of cyclones in the North Pacific. We study the variability of the field of surface
atmospheric pressure in different phases of the Pacific decadal oscillation characterizing the temperature anomalies on the
surface of the ocean in the region bounded by 20 and 60°N. It is shown that the decadal variations of the North Atlantic Oscillation
supported by the large-scale anomalies of the Pacific decadal oscillation is the most important cause of natural decadal oscillations
in the European region. We study and evaluate the regional response to the Pacific decadal oscillation by using, as an example,
the analysis of variations of the discharge of European rivers.
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Translated from Morskoi Gidrofizicheskii Zhurnal, No. 4, pp. 13–23, July–August, 2007. 相似文献
2.
Seasonal and interannual variability of the pressure field and indices of the North Atlantic atmosphere zonal circulation are analysed using historical (1894–1988) observations. It is shown that fluctuations of the index of North Atlantic oscillations (NAO) and that of the eastward transport give evidence of the interannual fluctuations with the typical time scale being 2–7 years. It is shown that the magnitude of interannual NAO index variability exceeds the typical magnitude of seasonal variations, particularly in winter. The time scale of NAO index variations and eastward transport coincides with the typicalEl Niño-southern oscillations (ENSO) temporal scale. The amplitudes of the annual, semi-annual harmonics, and high-frequency fluctuations of the NAO index increase during a typical ENSO event at least by a factor of 2.Translated by V. Puchkin. 相似文献
3.
E. N. Voskresenskaya A. S. Kukushkin N. V. Mikhailova 《Russian Meteorology and Hydrology》2011,36(1):45-54
The display is considered of global processes in the ocean-atmosphere system in the variability of hydrophysical and hydrobiological fields of the northwestern part of the Black Sea in spring period of 1978–1995. It is demonstrated that the variability of North Atlantic and Southern oscillations in winter-spring period affects the spring hydrometeorological conditions in catchment areas of European rivers of the Black Sea basin causing the variability of runoff volumes of these rivers and the scales of spreading river waters at the northwestern shelf. Hydrological and hydrobiological characteristics of shelf waters varying in the process influence the formation of distribution of suspended matter content and transparency. 相似文献
4.
N. P. Bulgakov R. A. Yaroshenya E. A. Skripaleva L. A. Voskresenskaya 《Physical Oceanography》2000,11(1):65-78
On the basis of the many-year-average seasonal data array of temperature and salinity presented on a scale of one-degree averaging,
by using a special quantitative criterion, we reveal a climatic frontal zone and determine both its physical and hydrological
characteristics (such as the length width, and thickness of the frontal layer and the temperature, salinity, and density gradients)
and its geographic coordinates. The many-year average seasonal variability of these characteristics is analyzed.
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
5.
N. P. Bulgakov R. A. Yaroshenya E. A. Skripaleva L. A. Voskresenskaya 《Physical Oceanography》2000,10(4):331-350
Climatic frontal zones are selected in the thermohaline fields of the Tropical Atlantic by analyzing the many-year-average
seasonal database reduced to the nodes of a one-degree grid. We determine physical characteristics of the frontal zones, study
their spatial and temporal variability, and reveal basic regularities of the appearance of frontal zones in the fields of
thermohaline characteristics.
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
6.
North Atlantic Oscillation: Description,Mechanisms, and Influence on the Eurasian Climate 总被引：1，自引：0，他引：1
Polonskii A. B. Basharin D. V. Voskresenskaya E. N. Worley S. 《Physical Oceanography》2004,14(2):96-113
The present work is devoted to the characteristic of the North-Atlantic Oscillation and the analysis of the state-of-the-art of this problem. In the survey section of the work, we deal with the following issues: the definition of the North Atlantic and Arctic Oscillations, their interaction with oceanic processes, and their influence on the variations of climate in Eurasia. In addition, by using the COADS (Comprehensive Ocean Atmosphere Data Set) data and the data on the discharge of European and Asian rivers, we establish some new original results. It is confirmed that the anomalies of the sea-surface temperature are consequences of the integral response of the ocean to the preceding atmospheric actions and that the spectra of these anomalies are characterized by the presence of significant peaks within the band of periods of 10–20 yr. These periods correspond to inherent oceanic variability. The atmospheric response manifests itself in the form of abnormal conditions over the catchment areas of European and Asian rivers, which leads to oscillations of their discharges. As a result of the intensification of the North Atlantic Oscillation and the displacement of the centers of action of the atmosphere in the 60–90s of the previous century, the influence of this oscillation on the climatic conditions in the European-Asian region became more intense. 相似文献
7.
The linear and quadratic trends of the parameters of interaction of the atmosphere with the ocean in the North Atlantic are computed according to the archival data of the Russian Hydrometeorological Center accumulated for 1957–1990. The linear trends are regarded as probable manifestations of the anthropogenic processes. At the same time, the quadratic trends are regarded as manifestations of natural low-frequency oscillations with a characteristic period of ~65 yr. The linear trends of the sea-surface temperature (SST) and the surface air temperature (SAT) are negative at high latitudes. The thermal (SST—SAT) contrasts and the deficiency of humidity E decrease over the most part of the investigated water area, thus revealing the active influence of the North Atlantic on the trends of SAT caused by the negative feedback in the system supported by the changes in the evident and latent heat fluxes. The significant quadratic trends of various hydrometeorological parameters and total heat fluxes confirm the predominance of natural variability with a period of ~65 yr in the North Atlantic. The quadratic trend of the heat fluxes is mainly caused by the quadratic trend of E. The coincidence of the phases of long-period anomalies of the SAT and E over the major part of the North Atlantic reveals the decisive role of the variability of the ocean in supporting the interdecadal oscillations in the ocean—atmosphere system.Translated from Morskoi Gidrofizicheskii Zhurnal, No. 4, pp. 19–38, July–August, 2004. 相似文献
8.
Polonskii A. B. Voskresenskaya E. N. Basharin D. V. Mikhailova N. V. 《Physical Oceanography》2003,13(3):171-182
On the basis of reanalysis of the data of the European Center of Medium-Range Weather Forecasts for 1979–1993, we study the relationship between the interannual and intramonthly variability of the fields of surface temperature and pressure in the Atlantic-European region and the Southern Oscillation (SO). In spring, the SO is responsible for 25% of the variance of surface temperature for periods of 8–30 days in the east part of Europe and in the Mediterranean region. In this case, the zonal circulation over the North Atlantic is intensified, which manifests itself in the deepening of the Iceland Low and Azores High. For low indices of SO, 8–15-day temperature fluctuations are predominant over the Black-Sea region. At the same time, 3–4-week fluctuations are predominant over West Mediterranean. An important role in the formation of abnormal temperature conditions in the analyzed region is payed by the events of La Niño. 相似文献
9.
A close correlation is found between dynamic processes in the near-earth tropical atmosphere, conditioned by air pressure anomalies in the Azor maximum, and the inter-annual ocean surface temperature variability in the north equatorial current area and in some other areas of the North Atlantic. A regression relation is proposed for calculating the sea surface temperature from the air pressure maximum in the Azor maximum. We discuss the anomalously high (low) upper ocean layer temperatures in the north equatorial current area induced by dynamic anomalies in the near-earth atmosphere and by the bottom topography.Translated by V. Puchkin. 相似文献
10.
N. P. Bulgakov R. A. Yaroshenya E. A. Skripaleva L. A. Voskresenskaya 《Physical Oceanography》1999,10(1):31-45
We determine the zones of maximum horizontal gradients of thermohaline characteristics and climatic frontal zones in the Tropical
Atlantic and their behavior as functions of time and spatial variables on the basis of the climatic array of data on temperature
and salinity. It is shown that the zones, where the maximum horizontal temperature, salinity, and density gradients coincide,
are located in the northern and southern tropical frontal zones.
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献