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Selin V. A. Emelyanov A. A. Sizov O. S. Emelyanov K. S. Borisov A. V. 《Izvestiya Atmospheric and Oceanic Physics》2020,56(9):1182-1189
Izvestiya, Atmospheric and Oceanic Physics - Our survey of various space image consumers identified that the geographic coverage, regularity, and frequency of observations are the most important... 相似文献
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Doğan Bülent Aşci Metin Karakaş Ahmet Pekşen Ertan Erener Arzu Çepni Murat Selim Yavuzyilmaz Selin Alahmad Mohammad Sertçelik Fadime Sertçelik İbrahim Kurtuluş Cengiz 《Natural Hazards》2021,109(2):1675-1716
Natural Hazards - The Northern Branch of the North Anatolian Fault System controls and deforms the Izmit Basin and the Sapanca Lake Basin in the study area. Unlike the Sapanca Lake Basin, the... 相似文献
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Süer Selin Wiersberg Thomas Güleç Nilgün Erzinger Jörg Parlaktuna Mahmut 《Natural Hazards》2020,104(2):1655-1678
Natural Hazards - This study presents the results of a real-time gas monitoring experiment conducted, via the use of a quadrupole mass spectrometer, in a mofette field within the Tekke Hamam... 相似文献
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Z. Liu R. G. Gallimore J. E. Kutzbach W. Xu Y. Golubev P. Behling R. Selin 《Climate Dynamics》1999,15(5):325-340
The use of the equilibrium asynchronous coupling (EAC) scheme is proposed as a strategy to better understand long-term climate
changes in a fully coupled ocean-atmosphere general circulation model. The EAC scheme requires each component model to be
integrated to its equilibrium before being coupled to the other component. Use of this scheme has the distinct advantage of
being able to clarify the nature of the coupling between the ocean and atmosphere, because each asynchronous iteration takes
the form of a sensitivity experiment. Basic features of the EAC scheme are first studied in an energy balance model. It is
found that the convergence rate of the EAC scheme is proportional to the damping rate in the atmosphere or surface ocean,
but is inversely proportional to the coupling strength between the ocean and atmosphere. Furthermore, the seasonal cycle response
converges much faster than the annual mean response. Using realistic parameters, the seasonal cycle response should converge
in a few iterations. The EAC scheme is further applied to a coupled ocean-atmosphere general circulation model to study the
tropical monsoon climate of the early Holocene. The convergence behavior of the sea surface temperature is found to agree
with the theory derived from the energy balance model study. The EAC scheme is further used to investigate the role of ocean-atmosphere
feedback in modifying the response of monsoons to orbital forcings in the early Holocene. It is found that the ocean exerts
a positive feedback on the North African monsoon, but a negative feedback on the Indian monsoon.
Received: 16 March 1998 / Accepted: 24 December 1998 相似文献
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Health damages from air pollution in China 总被引：1，自引：0，他引：1
Kira Matus Kyung-Min Nam Noelle E. Selin Lok N. Lamsal John M. Reilly Sergey Paltsev 《Global Environmental Change》2012,22(1):55-66
This study evaluates air pollution-related health impacts on the Chinese economy by using an expanded version of the Emissions Prediction and Policy Analysis model. We estimated that marginal welfare impact to the Chinese economy of ozone and particulate-matter concentrations above background levels increased from 1997 US$22 billion in 1975 to 1997 US$112 billion in 2005, despite improvements in overall air quality. This increase is a result of the growing urban population and rising wages that thus increased the value of lost labor and leisure. In relative terms, however, welfare losses from air pollution decreased from 14% of the historical welfare level to 5% during the same period because the total size of the economy grew much faster than the absolute air pollution damages. In addition, we estimated that particulate-matter pollution alone led to a gross domestic product loss of 1997 US$64 billion in 1995. Given that the World Bank's comparable estimate drawn from a static approach was only 1997 US$34 billion, this result suggests that conventional static methods neglecting the cumulative impact of pollution-caused welfare damage are likely to underestimate pollution-health costs substantially. However, our analysis of uncertainty involved in exposure–response functions suggests that our central estimates are susceptible to significantly large error bars of around ±80%. 相似文献
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Selin Süer Nilgün Güleç Halim Mutlu David R. Hilton Candan Çifter Mesut Sayin 《Pure and Applied Geophysics》2008,165(1):17-43
A total of nine geothermal fields located along an 800-km long E-W transect of the North Anatolian Fault Zone (NAFZ), Turkey were monitored for three years (2002–2004 inclusive; 3-sampling periods per year) to investigate any possible relationship between seismic activity and temporal variations in the chemistry and isotope characteristics of waters in the fields. The geothermal fields monitored in the study were, from west to east, Yalova, Efteni, Bolu, Mudurnu, Seben, Kur?unlu-Çank?r?, Hamamözü, Gözlek and Re?adiye. The chemical (major anion-cation contents) and isotopic (18O/16O, D/H, 3H) compositions of hot and cold waters of the geothermal sites were determined in order to both characterize the chemical nature of the individual fields and identify possible temporal variations associated with localized seismic activity. The geothermal waters associated with the NAFZ are dominantly Na-HCO3, whereas the cold waters are of the Ca-HCO3 type. The oxygen- and hydrogen-isotope compositions reveal that the hot waters are meteoric in origin as are their cold water counterparts. However, the lower δ18O, δD and 3H contents of the hot waters point to the fact that they are older than the cold waters, and that their host aquifers are recharged from higher altitudes with virtually no input from recent (post-bomb) precipitation. Although no major earthquakes (e.g., with M ≥ 5) were recorded along the NAFZ during the course of the monitoring period, variations in the chemical and isotopic compositions of some waters were observed. Indeed, the timing of the chemical/isotopic changes seems to correlate with the occurrence of seismic activity of moderate magnitude (3 < M < 5) close to the sampling sites. In this respect, Cl, 3H and Ca seem to be the most sensitive tracers of seismically-induced crustal perturbations, and the Yalova and Efteni fields appear to be the key localities where the effects of seismic activity on the geothermal fluids are most pronounced over the monitoring period. The present study has produced a ‘baseline’ database for future studies directed at characterizing the effects of moderate-major earthquakes on the composition of geothermal waters along the NAFZ. Future work involving longer monitoring periods with more frequent sampling intervals should lead to a better understanding of the underlying mechanism(s) producing the observed chemical and isotopic variations. 相似文献
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The 25th cruise of R/FAkademik Knipovitch conducted in January–April of 1990 comprised investigations of total organic carbon (TOC) at the following sections: through the Polar Frontal Zone (PFZ) along 40° W, made in January and April; from the PFZ to the South Orkney Islands, and on the South Georgia shelf. The measurements made comprised TOC, organic nitrogen, nitrate, nitrite, ammonium nitrogen, phosphate and silicate.The surface waters of the region were characterized by high heat content, which influenced the Antarctic phytosynosis function. The data obtained showed low content of organic matter (OM); high content of TOC, rising up to 3,5 mg m–3, was recorded at the photic layer and in the layer of OM accumulation, at the upper boundary of the Antarctic Deep Waters and the vertical boundaries of the Antarctic Intermediate Waters. The South Georgia shelf waters showed even distribution of TOC, about 0,2 mg m–3, being under the influence of the south periphery of the ACC waters. 相似文献
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