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11.
Summary In the past, experimental investigations as well as theoretical considerations have shown that within fronts and inversions wind shear and vertical temperature gradient adjust in such a way that the Richardson number is at its critical value. Results from aircraft measurements now suggest that the shear within moving cold fronts, warm fronts and inversions shows different behaviour because of the different mechanisms controlling the Richardson numbers. This leads to higher Richardson numbers, and therefore to lower amounts of wind shear within moving cold fronts when compared to warm fronts and inversions.With 9 Figures 相似文献
12.
C. Borries N. Jakowski Ch. Jacobi P. Hoffmann A. Pogoreltsev 《Journal of Atmospheric and Solar》2007,69(17-18):2442
The coupling of the neutral atmosphere and the ionosphere through planetary waves (PW) (zonal wavenumber 0–5) is investigated by spherical harmonic analyses of the ionospheric total electron content (TEC). These analyses detect mean variations, standing and travelling waves which are assumed to be signatures of PW. Database used for TEC analyses are 3 years of hourly TEC maps covering the higher middle and polar latitudes. They are regularly produced by DLR Neustrelitz. The obtained results are compared with PW analyses using NCEP/NCAR and Met Office stratospheric reanalyses. Case studies show that signatures of PW occur simultaneously in the middle atmosphere and ionosphere. 相似文献
13.
Ch. Jacobi P. Hoffmann R.Q. Liu P. Krian J. Las
tovi
ka E.G. Merzlyakov T.V. Solovjova Yu.I. Portnyagin 《Journal of Atmospheric and Solar》2009,71(14-15):1540-1546
We present time series of January–May mean mesosphere/lower thermosphere (MLT) mean winds and planetary wave (PW) proxies over Europe together with stratospheric stationary planetary waves (SPW) at 50°N and time series of European ozone laminae occurrence. The MLT winds are connected with stratospheric PW and laminae at time scales of several years to decades. There is a tendency for increased wave activity after 1990, together with more ozone laminae and stronger MLT zonal winds. However, possible coupling processes are not straightforward. While mean MLT winds before the 1990s show similar interannual variations than stratospheric PW at 100 hPa, later a tendency towards a connection of the MLT with the middle stratosphere SPW is registered. There is also a tendency for a change in the correlation between lower and middle stratosphere SPW, indicating that coupling processes involving the European middle atmosphere from the lower stratosphere to the mesopause region have changed. 相似文献
14.
E.G. Merzlyakov Ch. Jacobi Yu.I. Portnyagin T.V. Solovjova 《Journal of Atmospheric and Solar》2009,71(14-15):1547-1557
Recent analysis of the long-term behavior of different geophysical data has demonstrated that trend parameters can change during a period of observation. Sophisticated general methods for an objective analysis of structural changes in linear trends have been developed during the last 10 years. Such methods are applied for an analysis of changes in trend parameters of the mesosphere/lower thermosphere wind observed over Obninsk (55°N, 37°E) from 1964 to 2007 and Collm (52°N, 15°E) from 1979 to 2008, respectively. We found that trend models with breakpoints are generally preferred against straight lines. At Obninsk, there are break-years in trends of the winter prevailing winds close to 1977, when a climatic regime shift was observed. The break-years in trends of the semidiurnal tides for both stations are close to years of possible changes in stratospheric ozone. Correlations of the Obninsk and Collm winds with atmospheric indices are also considered. 相似文献
15.
C. Jacobi 《Theoretical and Applied Climatology》2000,65(3-4):231-243
Summary Investigation of long-term measurements of winter mesosphere/lower thermosphere (MLT) region zonal winds has shown a connection
of northern hemisphere tropospheric parameters and MLT conditions. These are on one hand due to a connection of the stratospheric
polar vortex and the North Atlantic Oscillation (NAO) and on the other hand forced by a coupling of the troposphere/lower
stratosphere and the MLT region through planetary wave propagation and wave-mean flow interaction. The connection between
European and Asian winter climatological parameters and the NAO leads to the fact, that the signal of Eurasian winter conditions
can be found in the interannual variability of MLT winds. Some of these winter tropospheric parameters influence the strength
of the Indian monsoon in the following summer, and this leads to a correlation between winter MLT winds and summer Indian
rainfall, so that the midlatitude MLT winter dynamics can be used as a precursory signal of the strength of the Indian monsoon.
Received July 21, 1998 Revised November 1, 1999 相似文献
16.
Gough's Cave is still Britain's most significant Later Upper Palaeolithic site. New ultrafiltered radiocarbon determinations on bone change our understanding of its occupation, by demonstrating that this lasted for only a very short span of time, at the beginning of the Lateglacial Interstadial (Greenland Interstadial 1 (GI-1: Bølling and Allerød)). The application of Bayesian modelling to the radiocarbon dates from this, and other sites from the period in southwest England, suggests that re-colonization after the Last Glacial Maximum took place only after 14,700 cal BP, and is, therefore, more recent than that of the Paris Basin and the Belgian Ardennes. On their own, the radiocarbon determinations cannot tell us whether re-colonization was synchronous with, just prior to, or after, Lateglacial warming. Isotopic studies of humanly-modified mammalian tooth enamel may be one way forward. 相似文献
17.
New TIMS dates from British sites underpin and extend the growing model of mammalian faunal history during the Late Pleistocene. The sequence of British faunas during the three successive warm phases of MIS 5 presents a challenging model in which the mammal faunas of the first two temperate phases, 5e and 5c is dominated by species of a classically interglacial character, while that of the final phase, sub‐stage 5a, is dominated by bison and reindeer. This we see as the ‘cold fauna’ appearing in Britain during the cool isotope sub‐stage 5b and subsequently isolated by the rising sea level of isotope sub‐stage 5a. All these three faunas are true island faunas. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献
18.
The presence of Eurasian lynx as a former native species in Britain during the Holocene is known from bones recovered from several sites. AMS radiocarbon dating of lynx bone recovered from two sites in the Craven area of northern England gave 1842 ± 35 14C yr BP and 1550 ± 24 14C yr BP, together representing the youngest dates for lynx from England, and in the case of the latter, the youngest for Britain as a whole. These dates support the view that the game animal whose occurrence in the nearby Lake District is described in the early 7th century Cumbric text Pais Dinogad, and whose translation to date has been problematic, is a lynx. The occurrence of lynx in early medieval Britain shows that earlier periods of climate change, previously blamed for the species' extinction in Britain, were not responsible. Instead, anthropogenic factors such as severe deforestation, declining deer populations, and persecution, are likely to have caused the extirpation of lynx in Britain. Consequently, the lynx qualifies as a candidate for reintroduction. Large‐scale reafforestation, the growth of deer populations, and more positive attitudes towards carnivores in modern society, could permit the restoration of lynx to Britain, particularly in Scotland. Copyright © 2005 John Wiley & Sons, Ltd. 相似文献
19.
The lunar semidiurnal tide in winds measured at around 90 km altitude has been isolated with amplitudes observed up to 4 m s–1. There is a marked amplitude maximum in October and also a considerable phase variation with season. The average variation of phase with height indicated a vertical wavelength of more than 80 km but this, and other results, needs to be viewed in the light of the considerable averaging required to obtain statistical significance. Large year-to-year variations in both amplitude and phase were also found. Some phase comparisons with the GSWM model gave reasonable agreement but the model amplitudes above a height of 100 km were much larger than those measured. An attempt to make a comparison with the lunar geomagnetic tide did not yield a statistically significant result. 相似文献
20.
W. Jacobi 《Pure and Applied Geophysics》1961,50(1):260-277
Zusammenfassung Es wird die Anlagerung der Zerfallsprodukte des, Radons und Thorons an das atmosphärische Aerosol infolge von Diffusion und elektrostatischer Dipolanziehung diskutiert. Die berechnete Grössenverteilung, des gebildeten, radioaktiven Aerosols stimmt weitgehend mit den Ergebnissen von Diffusionsmessungen überein. Die Aktivierung von Wolken-und Niederschlagselementen erfolgt im wesentlichen durch die Anlagerung trägerfreier, frisch gebildeter RaA-Atome; nur bei langlebigen Zerfallsprodukten spielt die Koagulation mit dem radioaktiven Aerosol eine Rolle. Die Anlagerungsgeschwindigkeit von RaA und ThB an fallende Regentropfen wurde durch Modellversuche bestimmt. Hiernach ist der Auswascheffekt von Regentropfen klein gegenüber der primären Aktivierung der Wolkenelemente. Es wird ein, Verfahren zur kontinuierlichen Messung der RaB- und RaC-Aktivität im Niederschlag beschrieben; die gemessene, mittlere spezifische Aktivität von 3·10–5 c/cm3 kann mit Hilfe der angegebenen Aktivierungsprozesse befriedigend erklärt werden.
Summary The attach of Rn- and Tn-decay-products to the atmospheric aerosol is discussed, taking into account diffusion and electrostatic forces. The computed size distribution of the produced radioactive aerosol agrees with the results of diffusion measurements. The activation of cloud and rain droplets with short-lived decay products happens chiefly due to the diffusion of fresh, carrier-free RaA-atoms. The collection efficiency of falling rain droplets for RaA and ThB was measured in model experiments; it is small compared to the activation of cloud elements. A method for the continuous measurement of RaB- and RaC-activity during rainfall is described; the measured, mean specific activity of 3·10–5 c/cm3 can be explained by the theory of activation processes.相似文献