An update on dynamical changes in the Arctic and Antarctic stratospheric polar vortices     

Ulrike Langematz  Markus Kunze 《Climate Dynamics》2006,27(6):647-660

Dynamical changes in the Arctic and Antarctic lower stratosphere from autumn to spring were analysed using the NCEP/NCAR, ERA40 and FUB stratospheric analyses for three periods: 1979–1999, 1979–2005, and 1965–2005. We found a weakening of the Arctic vortex in winter and a strengthening in spring between 1979/1980 and 1998/1999, with corresponding changes in the zonal mean circulation. The vortex formed earlier in autumn and broke down later in spring. These changes however were statistically not significant due to the high interannual dynamical variability in northern hemisphere (NH) winter and spring and the relatively short time series. In the Antarctic, the vortex formed earlier in autumn, intensified in late spring, and broke down later. The changes of the Antarctic vortex were at all levels and for both autumn and spring transitions larger and more significant than the changes of the Arctic vortex. These changes of the 1980s and early to mid 1990s were however not representative of a long-term change. The dynamically more active winters in the Arctic and Antarctic since 1998/1999 led to an enhanced weakening of the polar vortex in winter, and to a reduction of the polar vortex intensification in spring. As two of the recent Arctic major warmings occurred rather early in winter the polar vortex could recover in late winter and the delay in spring breakdown further increased. In contrast, the increase in Antarctic vortex persistence did no longer appear when including the recent winters due to the dominant impact of the three recent dynamically active Antarctic winters in 2000, 2002, and 2004. The long-term changes of 1965/1966–2005 were smaller in amplitude and partly opposite to the trends since the 1980s. There is no significant long-term change in the Arctic vortex lifetime or spring persistence, while the Antarctic vortex shows a long-term deepening and shift towards later spring transitions. The changes in the stratospheric dynamical situation could be attributed in both hemispheres to changes in the dynamical forcing from the troposphere.  相似文献   

An ostracod-conductivity transfer function for Tibetan lakes     

Steffen Mischke  Ulrike Herzschuh  Gudrun Massmann  Chengjun Zhang 《Journal of Paleolimnology》2007,38(4):509-524

About 145 freshwater to hypersaline lakes of the eastern Tibetan Plateau were investigated to develop a transfer function for quantitative palaeoenvironmental reconstructions using ostracods. A total of 100 lakes provided sufficient numbers of ostracod shells. Multivariate statistical techniques were used to analyse the influence of a number of environmental variables on the distributions of surface sediment ostracod assemblages. Of 23 variables determined for each site, 19 were included in the statistical analysis. Lake water electrical conductivity (8.2%), Ca% (7.6%) and Fe% (4.8%, ion concentrations as % of the cations) explained the greatest amounts of variation in the distribution of ostracod taxa among the 100 lakes. Electrical conductivity optima and tolerances were calculated for abundant taxa. A transfer function, based on weighted averaging partial least squares regression (WA-PLS), was developed for electrical conductivity (r ² = 0.71, root-mean-square-error of prediction [RMSEP] = 0.35 [12.4% of gradient length], maximum bias = 0.64 [22.4% of gradient length], as assessed by leave-one-out cross-validation) based on 96 lakes. Our results show that ostracods provide reliable estimates of electrical conductivity and can be used for quantitative palaeoenvironmental reconstructions similarly to more commonly used diatom, chironomid or pollen data.  相似文献   

Geostandards and Geoanalytical Research Bibliographic Review 2019     

Ulrike Weis  Brigitte Stoll  Jodok Arns  Michael W. Frster  Viktoria Kaiser  Laura M. Otter  Lea Reichstein  Klaus Peter Jochum 《Geostandards and Geoanalytical Research》2021,45(1):29-35

This bibliographic review gives an outline of publications in 2019 focusing on reference materials (RMs) used in geochemistry and related fields, such as palaeoclimate and environmental research.  相似文献   

Late Pleistocene to Holocene vegetation and climate changes in northwestern Chukotka (Far East Russia) deduced from lakes Ilirney and Rauchuagytgyn pollen records     

Andrei A. Andreev  Elena Raschke  Boris K. Biskaborn  Stuart A. Vyse  Jeremy Courtin  Thomas Böhmer  Kathleen Stoof-Leichsenring  Stefan Kruse  Lyudmila A. Pestryakova  Ulrike Herzschuh 《Boreas: An International Journal of Quaternary Research》2021,50(3):652-670

This paper presents two new pollen records and quantitative climate reconstructions from northern Chukotka documenting environmental changes over the last 27.9 ka. Open tundra- and steppe-like habitats dominated between 27.9 and 18.7 cal. ka BP. Betula and Alnus shrubs might have grown in sheltered microhabitats but disappeared after 18.7 cal. ka BP. Although the climate was rather harsh, local herb-dominated communities supported herbivores as is evident by the presence of coprophilous spores in the sediments. The increase in Salix and Cyperaceae ~16.1 cal. ka BP suggests climate amelioration. Shrub Betula appeared ~15.9 cal. ka BP, and became dominant after ~15.52 cal. ka BP, whilst typical steppe communities drastically reduced. Very high presence of Botryococcus in the Lateglacial sediments reflects widespread shallow habitats, probably due to lake level increase. Shrub Alnus became common after ~13 cal. ka BP reflecting further climate amelioration. Simultaneously, herb communities gradually decreased in the vegetation reaching a minimum ~11.8 cal. ka BP. A gradual decrease of algae remains suggests a reduction of shallow-water habitats. Shrubby and graminoid tundra was dominant ~11.8–11.1 cal. ka BP, later Salix stands significantly decreased. The forest-tundra ecotone established in the Early Holocene, shortly after 11.1 cal. ka BP. Low contents of green algae in the Early Holocene sediments likely reflect deeper aquatic conditions. The most favourable climate conditions were between ~10.6 and 7 cal. ka BP. Vegetation became similar to the modern after ~7 cal. ka BP but Pinus pumila came to the Ilirney area at about 1.2 cal. ka BP. It is important to emphasize that the study area provided refugia for Betula and Alnus during MIS 2. It is also notable that our records do not reflect evidence of Younger Dryas cooling, which is inconsistent with some regional environmental records but in good accordance with some others.  相似文献   

Antarctic shallow water benthos in an area of recent rapid glacier retreat          下载免费PDF全文

Francesca Pasotti  Elena Manini  Donato Giovannelli  Anne‐Cathrin Wölfl  Donata Monien  Elie Verleyen  Ulrike Braeckman  Doris Abele  Ann Vanreusel 《Marine Ecology》2015,36(3):716-733

The West Antarctic Peninsula is one of the fastest warming regions on Earth. Faster glacier retreat and related calving events lead to more frequent iceberg scouring, fresh water input and higher sediment loads, which in turn affect shallow water benthic marine assemblages in coastal regions. In addition, ice retreat creates new benthic substrates for colonization. We investigated three size classes of benthic biota (microbenthos, meiofauna and macrofauna) at three sites in Potter Cove (King George Island, West Antarctic Peninsula) situated at similar water depths but experiencing different disturbance regimes related to glacier retreat. Our results revealed the presence of a patchy distribution of highly divergent benthic assemblages within a relatively small area (about 1 km²). In areas with frequent ice scouring and higher sediment accumulation rates, an assemblage mainly dominated by macrobenthic scavengers (such as the polychaete Barrukia cristata), vagile organisms and younger individuals of sessile species (such as the bivalve Yoldia eightsi) was found. Macrofauna were low in abundance and very patchily distributed in recently ice‐free areas close to the glacier, whereas the pioneer nematode genus Microlaimus reached a higher relative abundance in these newly exposed sites. The most diverse and abundant macrofaunal assemblage was found in areas most remote from recent glacier influence. By contrast, the meiofauna showed relatively low densities in these areas. The three benthic size classes appeared to respond in different ways to disturbances likely related to ice retreat, suggesting that the capacity to adapt and colonize habitats is dependent on both body size and specific life traits. We predict that, under continued deglaciation, more diverse, but less patchy, benthic assemblages will become established in areas out of reach of glacier‐related disturbance.  相似文献   

Experimental subsolidus phase relations in the system CaCO3–CaMg(CO3)2 up to 6.5 GPa and implications for subducted marbles     

Jörg Hermann  Ulrike Troitzsch  Dean Scott 《Contributions to Mineralogy and Petrology》2016,171(10):84

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Long-term changes and solar impacts in the atmosphere–ionosphere system     

Gufran Beig  Jan Lastovicka  Ulrike Langematz 《Journal of Atmospheric and Solar》2009,71(13):1413-1414

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A closure study of sub-micrometer aerosol particle hygroscopic behaviour   总被引：2，自引：0，他引：2  

Erik Swietlicki  Jingchuan Zhou  Olle H. Berg  Bengt G. Martinsson  Gran Frank  Sven-Inge Cederfelt  Ulrike Dusek  Axel Berner  Wolfram Birmili  Alfred Wiedensohler  Brett Yuskiewicz  Keith N. Bower 《Atmospheric Research》1999,50(3-4)

The hygroscopic properties of sub-micrometer aerosol particles were studied in connection with a ground-based cloud experiment at Great Dun Fell, in northern England in 1995. Hygroscopic diameter growth factors were measured with a Tandem Differential Mobility Analyser (TDMA) for dry particle diameters between 35 and 265 nm at one of the sites upwind of the orographic cloud. An external mixture consisting of three groups of particles, each with different hygroscopic properties, was observed. These particle groups were denoted less-hygroscopic, more-hygroscopic and sea spray particles and had average diameter growth factors of 1.11–1.15, 1.38–1.69 and 2.08–2.21 respectively when taken from a dry state to a relative humidity of 90%. Average growth factors increased with dry particle size. A bimodal hygroscopic behaviour was observed for 74–87% of the cases depending on particle size. Parallel measurements of dry sub-micrometer particle number size distributions were performed with a Differential Mobility Particle Sizer (DMPS). The inorganic ion aerosol composition was determined by means of ion chromatography analysis of samples collected with Berner-type low pressure cascade impactors at ambient conditions. The number of ions collected on each impactor stage was predicted from the size distribution and hygroscopic growth data by means of a model of hygroscopic behaviour assuming that only the inorganic substances interacted with the ambient water vapour. The predicted ion number concentration was compared with the actual number of all positive and negative ions collected on the various impactor stages. For the impactor stage which collected particles with aerodynamic diameters between 0.17–0.53 μm at ambient relative humidity, and for which all pertinent data was available for the hygroscopic closure study, the predicted ion concentrations agreed with the measured values within the combined measurement and model uncertainties for all cases but one. For this impactor sampling occasion, the predicted ion concentration was significantly higher than the measured. The air mass in which this sample was taken had undergone extensive photochemical activity which had probably produced hygroscopically active material other than inorganic ions, such as organic oxygenated substances.  相似文献   

Einsatz von Pflanzenkläranlagen zur Behandlung von schadstoffbelastetem Oberflächenabfluß städtischer Straßen     

Susanne Osterkamp  Ulrike Lorenz  Michael Schirmer   《Limnologica》1999,29(1):93-102

A combination of retention pond and reed bed was tested for its effectiveness in reducing non-point source runoff pollution from an urban area. This paper presents data on the development of reed plants (Phragmites australis Cav. Trin.), on the effectiveness of runoff purification and on the accumulation of contaminants in the pond sediment and the reed bed for the years 1993–1995. P. australis was well established and grew according to normal development. The measured length and biomass values of P. australis were larger on sand than on gravel and coarse materials. Toxic levels of heavy metals in the plants were not reached. Harvested plants can be composted. The purification system is effective within the following ranges: The rate of retention of suspended solids and heavy metals varies between 16% and 91%. For chemical oxygen demand the average values is 25%. Poor retention rates usually occur along with very low input concentrations. Generally retention within the reed bed is higher than in the pond. Between 1993 and 1995 the concentration of contaminants within the organic layer of the reed bed increased by 50% for lead and by 90% for poly aromatic hydrocarbons. Until 1994 the concentrations of mineral oil hydrocarbons also increased by 60%. Between 1994 and 1995 however the concentration of mineral oil hydrocarbons in the reed bed decreased rapidly by more than 50%: Mineral oil hydrocarbons underlie biological degradation within the reed bed. In the pond sediment a significant accumulation of heavy metals, poly aromatic hydrocarbons and mineral oil hydrocarbons has also been found. The concentrations of these contaminants are still far from inhibiting the function of the system.  相似文献   

Zustandsentwicklung schleswig-holsteinischer Seen zwischen 1983 und 1993: Eine Betrachtung unter Anwendung der Clusteranalyse     

Gerald Schernewski  Ulrike Schulz 《Limnologica》1999,29(2):146

In 1983 the regional authority in Schleswig-Holstein (North Germany) started their long term monitoring programme in 29 lakes. During the following years the number increased to 68 lakes in 1993. The monitoring programme includes the parameter carbon (DOC, TOC), nitrogen (NH₄-N, NO₂-N, NO₃-N, TDN) phosphorus (PO₄-P, TDP), conductivity and temperature. Water samples are taken only once a year during late winter overturn in the main outflow of every lake. In this study TOC, TDN and TDP are chosen as most independent variables by correlation tests. Average concentrations of the years 1983 to 1985 and 1992 to 1993 as well as the concentration difference between 1992/93 and 1983/85 are clustered using the Average Linkage Method. It is necessary to use averages of a few years to reduce effects of interannual variability.Between 1983/85 and 1992/93 the average TDP-concentration in all 29 lakes was reduced by 40% from 0.68 to 0.041 mg/l. TDN-concentrations declined by 13% from 2.6 to 2.3 mg/l. The strong reduction of phosphorus concentrations clearly reflect the success of local sewage purification during the last two decades. The high importance of diffuse input sources for lakes is the reason for the less pronounced decline in TDN concentrations.The increase in TOC-concentrations by 14% (from 9.3 to 10.6 mg/l) between 1983/85 and 1992/93 is no indicator for an increased average annual algae biomass in the lakes. It is a result of unusual algae blooms during the warm winters between 1989 and 1993.Beside some similarities, the dendrogram on the basis of 1983/85 data and the one using 1992/93 values show that a lot of lakes are located to different clusters. The classification on the basis of concentration differences (1992/93–1983/85) yield three larger groups of lakes with a similar development and 5 groups containing only one or two lakes with extraordinary changes in their properties during the decade. To a certain degree, TOC, TDN and TDP can be seen as trophic state indicators. During the decade most lakes have been subject to significant changes and some main cluster with different directions of the trophic development become obvious. On the other hand a considerable number of lakes show a very special behaviour.The results underline that cluster methods are a useful tool to discover and analyse different developments in lakes. The calculation of T-values on the basis of classification results permit the identification of most representative individuals for every group of lakes. Representatives are valuable for a detailed discussion of driving forces and future investigations. They allow to handle a reduced number of lakes with minimal information loss about the entity.Lake Belau is the best representative for the average TOC-, TDN- and TDP-changes in all lakes. Its changes in water qualtity during the decade is discussed in detail. The high interannual variability of Chlorophyll a-, TDP- and TDN-concentrations in this lake clearly reflect the problems of long term analysis on the basis of this very limited monitoring programme.  相似文献