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1.
Geomagnetism and Aeronomy - It is shown that a source generating a slowly varying or quiet component of radio emission from ultracool stars such as the brown dwarf TVLM 513-46546 can be the... 相似文献
2.
Tsap Yu. T. Stepanov A. V. Kopylova Yu. G. Khaneichuk O. V. 《Geomagnetism and Aeronomy》2020,60(4):446-451
Geomagnetism and Aeronomy - The propagation of linear Alfvén waves with periods of 10–200 s from the photosphere to the solar chromosphere under the conditions of an isothermal... 相似文献
3.
Tatiana G. Elumeeva Vladimir G. Onipchenko Asem A. Akhmetzhanova Mikhail I. Makarov Joost A. Keuskamp 《山地科学学报》2018,15(8):1633-1641
Mountainous areas exhibit highly variable decomposition rates as a result of strong local differences in climate and vegetation type. This paper describes the effect of these factors on two major determinants of the local carbon cycle: litter decomposition and carbon stabilization. In order to adequately reflect local heterogeneity, we have sampled 12 typical plant communities of the Russian Caucasus. In order to minimize confounding effects and encourage comparative studies, we have adapted the widely used tea bag index (TBI) that is typically used in areas with low decomposition. By incubating standardized tea litter for a year, we investigated whether (1) initial litter decomposition rate (k) is negatively correlated with litter stabilization (S) and (2) whether k or S exhibit correlations with altitude and other environmental conditions. Our results show that S and k are not correlated. Altitude, pH, and water content significantly influenced the stabilization factor S, while soil-freezing had no influence. In contrast, none of these factors predicted the decomposition rate k. Based on our data, we argue that collection of decomposition rates alone, as is now common practice, is not sufficient to understand carbon input to soils and can potentially lead to misleading results. Our data on community-specific decomposition and stabilization rates further constrain estimates of litter accumulation in subalpine communities and the potential effects of climate change. 相似文献
4.
Vladimir V. Kukarskih Nadezhda M. Devi Pavel A. Moiseev Andrey A. Grigoriev Maksim O. Bubnov 《山地科学学报》2018,15(4):722-729
This paper presents a dendroclimatic analysis of Siberian larch trees sampled along a latitudinal 260-km transect located in the Polar Urals,Russia. Three standardised chronologies were built over a length of 230–293 years using 79 individual tree-ring chronologies collected in the southern,middle and northern parts of the Polar Urals.Bootstrapped correlation functions showed that the annual growth of the larches was mainly influenced by the air temperatures in June and July. The relative role of the temperatures increased from south to north. Daily air temperature data analysis revealed that the duration of the growing season in the northern part of the Polar Urals is 24 days less than that in the southern part. At the present time, air temperatures exceeded threshold of 8~℃, 5 days earlier than it did in the beginning of the 20 th century In response to the increase in the duration of the growing season and the changing winter conditions in the Polar Urals over the last 130 years, radial growth–temperature relationships in larches have weakened;this effect was strongly pronounced in the southern part of the Polar Urals. 相似文献
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Ayupova N. R. Maslennikov V. V. Tseluyko A. S. Stepanov A. V. Artemyev D. A. Belogub E. V. Kotlyarov V. A. Butnyakov A. V. 《Geology of Ore Deposits》2021,63(1):79-86
Geology of Ore Deposits - Pyrite ores on the flanks of the Saum copper–zinc massive sulfide deposit are clastic sediments intensely transformed under conditions of acid diagenesis. Colusite... 相似文献
9.
The hourly data of nine geomagnetic observatories situated in Central Europe have been analyzed using the generalized magnetovariation
(GMV) method designed recently for induction soundings of inhomogeneous media. In this method, impedance is one of transfer
functions in the differential relation between spectra of the magnetic components and their derivatives. The peculiarity of
this impedance is its correspondence to the magnetotelluric one estimated from the linear relations. Three transfer functions
have been estimated simultaneously for data of geomagnetic observatories, using three different routines working in the period
range from three hours up to two days. Noises in the source field components have been compared with noise in the estimated
plane field divergence. The multivariate errors-in-variables method was used to extract spatially and temporally coherent
geomagnetic field structure from the partially incoherent geomagnetic variations. This method allows estimating reliably impedances
and gradient tippers for each observatory, taking into consideration the Earth’s sphericity. The obtained responses have been
used for induction soundings and for detecting a deep inhomogeneity in the region. 相似文献
10.
William L. Bandy Yuri Taran Carlos Mortera Guti��rrez Vladimir Kostoglodov 《Pure and Applied Geophysics》2011,168(8-9):1251-1253