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Trace elemental concentrations of bivalve shells content a wealthy of environmental and climatic information of the past, and therefore the studies of trace elemental distributions in bivalve shells gained increasing interest lately. However, after more than half century of research, most of the trace elemental variations are still not well understood and trace elemental proxies are far from being routinely applicable. This dissertation focuses on a better understanding of the trace elemental chemistry of Arctica islandica shells from Iceland, and paving the way for the application of the trace elemental proxies to reconstruct the environmental and climatic changes. Traits of trace elemental concentrations on A. islandica shells were explored and evaluated. Then based the geochemical traits of the shells, four non-environmental/climatic controlling is indentified. (1) Trace elemental concentrations of bivalve shells are effected by early diagenesis by the leach or exchange of elemental ions, especially in shell tip part, even with the protection of periostrucum; (2) The analytical methods also affect the results of trace elemental concentrations, especially for the element, such as Mg, which is highly enriched in organic matrices; (3) Shell organic matrices are found play a dominating role on the concentration of trace elements on A. islandica shells. Most trace elements only occurred in insoluble organic matrices (IOM), although others are only found in the carbonate fraction. IOM of A. islandica shells is significantly enriched in Mg, while Li and Na are more deplete in IOM, but enriched in shell carbonate. Ba is more or less even contented in IOM and shell carbonate. The concentrations of certain elements vary between primary layer and secondary layer; (4) The vital /physiological controlling on trace elemental distributions of bivalve shells is also confirmed. Six elemental (B, Na, Mg, Mn, Sr, and Ba) concentrations show significant correlation (exponential functions) with ontogenetic age and shell grow rates (logarithmic equations). It is worthy to remark that B, Mg, Sr and Ba concentrations are negatively correlated with shell growth rate, positive with ontogenetic age, while the concentrations of Na and Mn show the opposite trends. At last, all the controlling described above can be taken into account and corrected to extract the environmental and climatic signal by a kind of standardization. The derived six exponential functions of the high correlations between six trace elemental concentrations and ontogenetic year are applied to make the standardization of these element-Ca ratios. The gotten standardized indices are compared with the variations of environmental and climatic parameters in this region, and many correlations are found. Standardized indices of Sr/Ca ratios are strongly related to the sun spot number, autumn NAO, autumn Europe surface air temperature (SAT) and Arctic sea surface temperature anomaly (TA), and those of Mg/Ca ratios are strongly associated with Arctic TA, Europe SAT and Solar variation (irradiance). The variations of autumn Europe SAT demonstrated more similarity with standardized indices of B/Ca than other parameters. Except for the SAT index of Arctic, the standardized indices of Na/Ca showed no distinct relation to temperature. European precipitation and the Arctic sea level pressure index compared well the Na/Ca ratios of the shells, and so did the autumn NAO. Standardized indices of Mn/Ca were correlated with the number of hurricanes in the North Atlantic, Northern Europe SAT and sun spot number.
Samples of freshly fallen snow were collected at the high alpine research station Jungfraujoch (Switzerland) in February and March 2006 and 2007, during the Cloud and Aerosol Characterization Experiments (CLACE) 5 and 6. In this study a new technique has been developed and demonstrated for the measurement of organic acids in fresh snow. The melted snow samples were subjected to solid phase extraction and resulting solutions analysed for organic acids by HPLC-MS-TOF using negative electrospray ionization. A series of linear dicarboxylic acids from C5 to C13 and phthalic acid, were identified and quantified. In several samples the biogenic acid pinonic acid was also observed. In fresh snow the median concentration of the most abundant acid, adipic acid, was 0.69 micro g L -1 in 2006 and 0.70 micro g L -1 in 2007. Glutaric acid was the second most abundant dicarboxylic acid found with median values of 0.46 micro g L -1 in 2006 and 0.61 micro g L -1 in 2007, while the aromatic acid phthalic acid showed a median concentration of 0.34 micro g L -1 in 2006 and 0.45 micro g L -1 in 2007. The concentrations in the samples from various snowfall events varied significantly, and were found to be dependent on the back trajectory of the air mass arriving at Jungfraujoch. Air masses of marine origin showed the lowest concentrations of acids whereas the highest concentrations were measured when the air mass was strongly influenced by boundary layer air.
Active chlorine species play a dominant role in the catalytic destruction of stratospheric ozone in the polar vortices during the late winter and early spring seasons. Recently, the correct understanding of the ClO dimer cycle was challenged by the release of new laboratory absorption cross sections (Pope et al., 2007) yielding significant model underestimates of observed ClO and ozone loss (von Hobe et al., 2007). Under this aspect, Arctic stratospheric limb emission measurements carried out by the balloon version of the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS-B) from Kiruna (Sweden) on 11 January 2001 and 20/21 March 2003 have been reanalyzed with regard to the chlorine reservoir species ClONO2 and the active species, ClO and ClOOCl (Cl2O2). New laboratory measurements of IR absorption cross sections of ClOOCl for various temperatures and pressures allowed for the first time the retrieval of ClOOCl mixing ratios from remote sensing measurements. High values of active chlorine (ClOx) of roughly 2.3 ppbv at 20 km were observed by MIPAS-B in the cold mid-winter Arctic vortex on 11 January 2001. While nighttime ClOOCl shows enhanced values of nearly 1.1 ppbv at 20 km, ClONO2 mixing ratios are less than 0.1 ppbv at this altitude. In contrast, high ClONO2 mixing ratios of nearly 2.4 ppbv at 20 km have been observed in the late winter Arctic vortex on 20 March 2003. No significant ClOx amounts are detectable on this date since most of the active chlorine has already recovered to its main reservoir species ClONO2. The observed values of ClOx and ClONO2 are in line with the established chlorine chemistry. The thermal equilibrium constants between the dimer formation and its dissociation, as derived from the balloon measurements, are on the lower side of reported data and in good agreement with values recommended by von Hobe et al. (2007). Calculations with the ECHAM/MESSy Atmospheric Chemistry model (EMAC) using established kinetics show similar chlorine activation and deactivation, compared to the measurements in January 2001 and March 2003, respectively.
A characterization of the ultra-fine aerosol particle counter COPAS (COndensation PArticle counting System) for operation on board the Russian high altitude research aircraft M-55 Geophysika is presented. The COPAS instrument consists of an aerosol inlet and two dual-channel continuous flow Condensation Particle Counters (CPCs) operated with the chlorofluorocarbon FC-43. It operates at pressures between 400 and 50 hPa for aerosol detection in the particle diameter (dp) range from 6 nm up to 1 micro m. The aerosol inlet, designed for the M-55, is characterized with respect to aspiration, transmission, and transport losses. The experimental characterization of counting efficiencies of three CPCs yields dp50 (50% detection particle diameter) of 6 nm, 11 nm, and 15 nm at temperature differences (DeltaT) between saturator and condenser of 17°C, 30°C, and 33°C, respectively. Non-volatile particles are quantified with a fourth CPC, with dp50=11 nm. It includes an aerosol heating line (250°C) to evaporate H2SO4-H2O particles of 11 nm<dp<200 nm at pressures between 70 and 300 hPa. An instrumental in-flight inter-comparison of the different COPAS CPCs yields correlation coefficients of 0.996 and 0.985. The particle emission index for the M-55 in the range of 1.4–8.4×10 16 kg -1 fuel burned has been estimated based on measurements of the Geophysika's own exhaust.
Volatile organic compounds (VOCs) were analyzed in air and snow samples at the Jungfraujoch high alpine research station in Switzerland as part of CLACE 5 (CLoud and Aerosol Characterization Experiment) during February/March 2006. The fluxes of individual compounds in ambient air were calculated from gas phase concentrations and wind speed. The highest concentrations and flux values were observed for the aromatic hydrocarbons benzene (14.3 μg.m−2 s−1), 1,3,5-trimethylbenzene (5.27 μg.m−2 s−1), toluene (4.40 μg.m−2 −1), and the aliphatic hydrocarbons i-butane (7.87 μg.m−2 s−1), i-pentane (3.61 μg.m−2 s−1) and n-butane (3.23 μg.m−2 s−1). The measured concentrations and fluxes were used to calculate the efficiency of removal of VOCs by snow, which is defined as difference between the initial and final concentration/flux values of compounds before and after wet deposition. The removal efficiency was calculated at −24°C (−13.7°C) and ranged from 37% (35%) for o-xylene to 93% (63%) for i-pentane. The distribution coefficients of VOCs between the air and snow phases were derived from published poly-parameter linear free energy relationship (pp-LFER) data, and compared with distribution coefficients obtained from the simultaneous measurements of VOC concentrations in air and snow at Jungfraujoch. The coefficients calculated from pp-LFER exceeded those values measured in the present study, which indicates more efficient snow scavenging of the VOCs investigated than suggested by theoretical predictions.
We use observations of total particle number concentration at 36 worldwide sites and a global aerosol model to quantify the primary and secondary sources of particle number. We show that emissions of primary particles can reasonably reproduce the spatial pattern of observed condensation nuclei (CN) (R2=0.51) but fail to explain the observed seasonal cycle at many sites (R2=0.1). The modeled CN concentration in the free troposphere is biased low (normalised mean bias, NMB=−88%) unless a secondary source of particles is included, for example from binary homogeneous nucleation of sulfuric acid and water (NMB=−25%). Simulated CN concentrations in the continental boundary layer (BL) are also biased low (NMB=−74%) unless the number emission of anthropogenic primary particles is increased or an empirical BL particle formation mechanism based on sulfuric acid is used. We find that the seasonal CN cycle observed at continental BL sites is better simulated by including a BL particle formation mechanism (R2=0.3) than by increasing the number emission from primary anthropogenic sources (R2=0.18). Using sensitivity tests we derive optimum rate coefficients for this nucleation mechanism, which agree with values derived from detailed case studies at individual sites.
Samples of freshly fallen snow were collected at the high alpine research station Jungfraujoch, Switzerland, during the Cloud and Aerosol Characterization Experiments (CLACE) 5 in February and March 2006. Sampling was carried out on the Sphinx platform. Headspace-solid-phase-dynamic extraction (HS-SPDE) combined with gas chromatography/mass spectrometry (GC/MS) was used to quantify C6–C10 n-aldehydes in the snow samples. The most abundant n-aldehyde was n-hexanal (median concentration 1.324 micro g L -1) followed by n-nonanal, n-decanal, n-octanal and n-heptanal (median concentrations 1.239, 0.863, 0.460, and 0.304 micro g L -1, respectively). A wide range of concentrations was found among individual snow samples, even for samples taken at the same time. Higher median concentrations of all n-aldehydes were observed when air masses reached Jungfraujoch from the north-northwest in comparison to air masses arriving from the southeast-southwest. Results suggest that the n-aldehydes detected most likely are of direct and indirect biogenic origin, and that they entered the snow through the particle phase.
The present PhD-thesis was prepared within subproject B8 of the DFG-Sonderforschungsbereich (SFB) 641 “The Tropospheric Ice Phase”. The subproject B8 was entitled “Interactions of volatile organic compounds with airborne ice crystals”. Results of previous studies have shown that various volatile organic compounds (VOC) and semivolatile organic compounds (SVOC) are incorporated into the atmospheric ice phase and several uptake mechanisms are discussed in the literature. The aim of this study was to identify the dominating VOC and SVOC in airborne snow collected at Jungfraujoch in the Swiss Alps (3580 m asl) and to study in laboratory experiments the uptake mechanism of organic compounds into snow and ice. For this purpose an analytical method to analyse freshly fallen snow samples was developed and evaluated in a first step. The method consists of headspace (HS) solid phase dynamic extraction (SPDE) followed by gas chromatography combined with mass spectrometry (GC/MS). During the extraction process a new cooling device was successfully integrated into the HS-SPDE-GC/MS method to enhance the extraction yield. Extraction and desorption parameters such as the number of extraction cycles, extraction temperature, desorption volume and desorption flow rate have been optimized. Detection limits for benzene, toluene, ethylbenzene, m-, p-, o- xylene (BTEX) ranged from 19 ng L-1 (benzene) to 30 ng L-1 (m/p-xylene), while those for C6-C10 n-aldehydes ranged from 21 ng L-1 (n-heptanal) to 63 ng L-1 (n-hexanal). Furthermore, freshly fallen snow samples were collected at the High Altitude Research Station Jungfraujoch (3580 m asl, Switzerland) during the field campaigns “Cloud and aerosol characterization experiment” (CLACE) 4 and 5 in February and March 2005 and 2006, respectively. Freshly fallen snow samples collected directly in-cloud on a high altitude remote location were used as approximation of airborne ice crystals since sampling of airborne ice crystals in quantities sufficient for analysis of individual organic compounds is not yet possible. In the collected snow samples a wide range of organic compounds were identified, namely BTEX, n-aldehydes (C6-C10), terpenes, chlorinated hydrocarbons and alkylated monoaromatics. The most abundant organic compounds in snow samples from Jungfaujoch during CLACE 4 and 5 were n-hexanal with a median concentration of 1.324 μg L-1 (CLACE 5) followed by n-nonanal (CLACE 5) with a median concentration of 1.239 μg L-1. High concentration variations of the analytes in snow samples collected at the same time at the same place argue for a heterogeneous composition of snow and ice. Several indicators were found that the origin of the n-aldehydes in the snow can be attributed to direct biogenic emissions from vegetation and indirect biogenic emissions through photochemical oxidation of fatty acids and alkenes. In a second step laboratory experiments were carried out to clarify the uptake mechanism of volatile and semivolatile organic compounds into snow/ice. Organic compounds can be incorporated into the atmospheric ice phase either by the process of gas scavenging, liquid scavenging (riming) or particle scavenging. Gas scavenging (incorporation of the organic compounds from the gas phase during growing of ice crystals) revealed to be ineffective based on previous laboratory experiments in which ice crystals were growing in the presence of aromatic hydrocarbons (BTEX) in the gas phase. In the present study the process of liquid scavenging (riming) was investigated in the laboratory using aqueous standard solutions containing BTEX, naldehydes (C6-C10), methyl tert-butyl ether (MTBE) and ethyl tert-butyl ether (ETBE). The headspace above the standard solution was sampled after adjusting the aqueous solutions to definite temperatures by use of a thermostat. Measurement were carried out at 25°C, 15°C and 5°C (water), -5°C and -15°C (supercooled water) and -25°C (ice). Results have shown that the known trend of lower gas phase concentrations over water concomitant with lower temperatures (Henry’s Law) is only valid for temperatures above 0°C. At temperature below 0°C, increasing concentrations of the analytes (BTEX, MTBE, ETBE and n-aldehydes) were determined in the gas phase together with decreasing temperatures. Dimensionless Henry’s law coefficients (KAW) were calculated from the concentrations of the organic compounds in the headspace above the standard solutions at temperatures between 25°C and -25°C. The observed inversion of Henry’s law coefficients of volatile and semivolatile organic compounds at a water temperature of approximately 0°C is explained by the formation of ordered zones of H2O molecules in supercooled water called “ice-like-clusters”. Together with decreasing temperatures the degree of formation of ordered zones increases which results in the removal of the organic molecules from the liquid phase and transfer into the gas phase. At a temperature of -25°C the supercooled water is converted into ice and a further significant increase of the gas phase concentrations of hydrophobic compounds such as BTEX is observed. In comparison, less hydrophobic compounds such as MTBE, ETBE and n-aldehydes are detected in lower amounts in the gas phase above the water/ice phase due to the higher water solubility and lower Henry coefficients compared to BTEX. The results show that in the absence of particles the uptake of BTEX MTBE, ETBE and C6-C10-naldehydes into ice not enhanced during freezing of a supercooled liquid, since at -25°C for these analytes the concentrations in the gas phase are higher at -25°C (ice) compared with -15°C (supercooled liquid). The heterogeneous distribution of BTEX and n-aldehydes concentrations in snow samples collected during the CLACE field campaigns suggests that adsorption of the organic compounds to particles followed by incorporation of the particles into the snow and ice might play a major role in the uptake process of organic compounds into snow and ice. To increase the knowledge about uptake processes of organic compounds into snow and ice further experiments are required with should include aerosol particles in the experimental setup to evaluate the influence of particle scavenging in the uptake processes.
Delthyridoid spiriferids are characterized by a global abundance and fast evolution during Silurian and Devonian, and, therefore, are used as important biostratigraphical and palaeobiogeographical tools. In this work, delthyridoid brachiopod faunas from different regions of today’s world, resp., of different palaeobiogeographical units, are compared side-by-side to investigate their phylogenetic relationships and to improve, in a second step, the palaeobiogeography from Late Silurian to Early Eifelian time. A new systematics of Delthyridoidae is established which is more complicated than hitherto assumed. The results of this study are mainly based on direct comparison of articulated and isolated brachiopod shells, external and internal moulds, as well as latex casts and serial sections. The computer supported cladistic analyses have turned out not to be useful due to different kinds of preservation resulting in an incomplete matrix which is insufficient for reliable cladograms. A further problem in terms of cladistical analyses are various convergences during the evolution of spiriferids. Many characters evolved independently from each other at different times in each lineage so that autapomorphies are hardly or not at all recognizable. As a result, families and genera are only definable by a combination of characters rather than by a single or a few autapomorphies. As a new method, 3D reconstruction from serial sections is introduced which made it possible for the first time to compare directly mouldic and shelly material. Preliminary results are presented herein. Statistical analyses of measurements taken from new taxa are made but regarded as a descriptive argument rather than a deciding factor for taxonmy due to incomplete preservation and/or tectonic deformation. Brachiopods, especially type material, from collections of different institutions and museums are studied as well as personal material, whenever possible collected from topotype outcrops. Emended diagnoses, if necessary, from family to species level are given. During this work several new taxa have been erected: 7 new families: Australospiriferidae, Murchisonispiriferidae, Orientospiriferidae, Otospiriferidae, Patriaspiriferidae, Rostrospiriferidae, and Trigonospiriferidae; 6 new genera, 1 of these in open nomenclature: Cyclopterospirifer, Hallispirifer, Parlinispirifer, Murchisonispirifer, Shujiapingensispirifer, and gen. nov. B; and 3 new species: Patriaspirifer merriami, Patriaspirifer johnsoni, and Murchisonispirifer feldmani; 1 taxon is defined as nomen novum: Orientospirifer nakaolingensis wani. In the framework of this project, 2 families: Filispiriferidae and Multispiriferidae; 1 subfamily: Multiplicatispiriferinae, 6 genera, 1 of them in open nomenclature: Frequentispirifer, Leonispirifer, Multiplicatispirifer, Ovetensispirifer, Turcispirifer, and Gen. A; and 9 new species, 3 of them in open nomenclature: Filispirifer hamadae, Leonispirifer leonensis, Multiplicatispirifer foumzguidensis, Oventensispirifer novascotianus, Quiringites arensentiae, Turcispirifer turciae, Multiplicatispirifer cf. foumzguidensis, Quiringites cf. arensentiae, and ?Turcispirifer sp. A which have already been established are also described in this work. The brachiopod faunas studied consist of externally very similar spiriferids which have been identified as same genera, species, or even subspecies in earlier times. These forms are considered as 6 distinct morphotypes Howellella-, Arduspirifer-, Acrospirifer-, Euryspirifer-, Paraspirifer-, and Multiplicatispirifer-like morphotypes, which are briefly introduced. The new systematics is characterized by different clades, the European/North African delthyridoid spiriferid clade, the North American delthyridoid spiriferid clade, the Asian delthyridoid spiriferid clade, the Malvinokaffric delthyridoid spiriferid clade, and the delthyridoid multiplicated spiriferid clade. Each of them is described in a cladistic and in a phylogenetic way. Their phylogenetic relationship sheds new light on palaeobiogeographical interpretations for the different stages from Late Silurian to early Middle Devonian time. A tendency for increasing endemicity is seen until the end of the Early Emsian, which is interrupted by short term regional faunal exchange within a province or within a realm, followed by a loss of endemicity resulting in global distribution of brachiopod genera until the end of Givetian time. The Old World Realm is re-defined due to the lack of phylogenetic relationship between its faunas and subdivided into the European Realm, consisting of the Gondwanan and Avalonian provinces, and the Asian Realm, consisting of the Siberian, Sino, and Mongolian provinces. A reconstruction of Lower Devonian palaeobiographical map is introduced.
The ENVISAT validation programme for the atmospheric instruments MIPAS, SCIAMACHY and GOMOS is based on a number of balloon-borne, aircraft, satellite and ground-based correlative measurements. In particular the activities of validation scientists were coordinated by ESA within the ENVISAT Stratospheric Aircraft and Balloon Campaign or ESABC. As part of a series of similar papers on other species [this issue] and in parallel to the contribution of the individual validation teams, the present paper provides a synthesis of comparisons performed between MIPAS CH4 and N2O profiles produced by the current ESA operational software (Instrument Processing Facility version 4.61 or IPF v4.61, full resolution MIPAS data covering the period 9 July 2002 to 26 March 2004) and correlative measurements obtained from balloon and aircraft experiments as well as from satellite sensors or from ground-based instruments. In the middle stratosphere, no significant bias is observed between MIPAS and correlative measurements, and MIPAS is providing a very consistent and global picture of the distribution of CH4 and N2O in this region. In average, the MIPAS CH4 values show a small positive bias in the lower stratosphere of about 5%. A similar situation is observed for N2O with a positive bias of 4%. In the lower stratosphere/upper troposphere (UT/LS) the individual used MIPAS data version 4.61 still exhibits some unphysical oscillations in individual CH4 and N2O profiles caused by the processing algorithm (with almost no regularization). Taking these problems into account, the MIPAS CH4 and N2O profiles are behaving as expected from the internal error estimation of IPF v4.61 and the estimated errors of the correlative measurements.
A suite of diagnostics is applied to in-situ aircraft measurements and one Chemistry-Climate Model (CCM) data to characterize the vertical structure of the Tropical Tropopause Layer (TTL). The diagnostics are based on vertical tracer profiles and relative vertical tracer gradients, using tropopause-referenced coordinates, and tracer-tracer relationships in the tropical Upper Troposphere/Lower Stratosphere (UT/LS).
Observations were obtained during four tropical campaigns performed from 1999 to 2006 with the research aircraft Geophysica and have been compared to the output of the ECHAM5/MESSy CCM. The model vertical resolution in the TTL (~500 m) allows for appropriate comparison with high-resolution aircraft observations and the diagnostics used highlight common TTL features between the model and the observational data.
The analysis of the vertical profiles of water vapour, ozone, and nitrous oxide, in both the observations and the model, shows that concentration mixing ratios exhibit a strong gradient change across the tropical tropopause, due to the role of this latter as a transport barrier and that transition between the tropospheric and stratospheric regimes occurs within a finite layer. The use of relative vertical ozone and carbon monoxide gradients, in addition to the vertical profiles, helps to highlight the region where this transition occurs and allows to give an estimate of its thickness. The analysis of the CO-O3 and H2O-O3 scatter plots and of the Probability Distribution Function (PDF) of the H2O-O3 pair completes this picture as it allows to better distinguish tropospheric and stratospheric regimes that can be identified by their different chemical composition.
The joint analysis and comparison of observed and modelled data allows to state that the model can represent the background TTL structure and its seasonal variability rather accurately. The model estimate of the thickness of the interface region between tropospheric and stratospheric regimes agrees well with average values inferred from observations. On the other hand, the measurements can be influenced by regional scale variability, local transport processes as well as deep convection, that can not be captured by the model.
A suite of diagnostics is applied to in-situ aircraft measurements and one Chemistry-Climate Model (CCM) data to characterize the vertical structure of the Tropical Tropopause Layer (TTL). The diagnostics are based on the vertical tracers profiles, relative vertical tracers gradients, and tracer-tracer relationships in the tropical Upper Troposphere/Lower Stratosphere (UT/LS), using tropopause coordinates.
Observations come from the four tropical campaigns performed from 1998 to 2006 with the research aircraft Geophysica and have been directly compared to the output of the ECHAM5/MESSy CCM. The model vertical resolution in the TTL allows for appropriate comparison with high-resolution aircraft observations and the diagnostics used highlight common TTL features between the model and the observational data.
The analysis of the vertical profiles of water vapour, ozone, and nitrous oxide, in both the observations and the model, shows that concentration mixing ratios exhibit a strong gradient change across the tropical tropopause, due to the role of this latter as a transport barrier and that transition between the tropospheric and stratospheric regimes occurs within a finite layer. The use of relative vertical ozone gradients, in addition to the vertical profiles, helps to highlight the region where this transition occurs and allows to give an estimate of its thickness. The analysis of the CO-O3 and H2O-O3 scatter plots and of the Probability Distribution Function (PDF) of the H2O-O3 pair completes this picture as it allows to better distinguish tropospheric and stratospheric regimes that can be identified, first, by their differing chemical composition.
The joint analysis and comparison of observed and modelled data allows us to evaluate the capability of the model in reproducing the observed vertical structure of the TTL and its variability, and also to assess whether observations from particular regions on a monthly timescale can be representative of the fine scale mean structure of the Tropical Tropopause Layer.
New industries are recognized as new impetus to national wealth. At the same time, they are increasingly becoming geographically concentrated in some well defined areas. But current studies on the emergence of industrial clusters tend to analyze favorable driving factors. This dissertation takes the example of a Chinese endogenous industrial cluster, the traditional Chinese medicine (TCM) cluster at Tonghua, a small peripheral city in Northeastern China, to contribute to the theoretical understanding of the emergence of industrial cluster as a co-evolutionary process of organizations, institutions and firms, or, to put it more broadly, as economic evolution embedded in complex socio-economic contexts. The recent advance in evolutionary and co-evolutionary economics which considers the economy and economic landscape as dynamic process instead of equilibrium can be regarded as a part of broader and more intellectual turn of quest for history in social sciences. Although the principle of "history matters" is widely acknowledged, it tends to be reduced to a quite simple concept of "path dependence". However, path dependence cannot offer space for new path creation, except from an external shock. Accordingly, the role of human conscious action or Schumpeterian innovation should be added to path analysis through the concept of path creation. Furthermore, and more importantly, history should be understood as context, and historical context can be explored through the understanding of multi-paths and interaction among them over time. So path inter-dependence (co-evolution between paths) would be useful to better understand the complexity of real history. Since the industrial cluster is composed of interconnected firms and is also subject to changes in institution and technology, I will focus on the multi-way causal relationship between firm, institution and technology. The theorizing is not entirely new, but most of the theoretical and empirical discussions are at the national or industrial level, not regional or local one. A competitive cluster can be regarded as a co-evolutionary hotspot in which multiple populations actively interact and are interconnected. Co-evolution itself is a dynamic and evolutionary process. So I will adopt a dynamic and evolutionary view to examine co-evolutionary degree or co-evolutionary effects in the Tonghua pharmaceutical cluster through time. After a brief introduction which deals with the national institutional changes that are highly associated with new venture creation, entrepreneurship, and innovation, with registrations on drug and healthcare system, and with changes in market demand of China’s pharmaceutical industry and geographical distribution, I will collect evidences from three aspects based upon field survey and second hand data, i.e., the history of the enterprises, the origin of entrepreneurship, and the knowledge of evolution, linking their respective generative relationships through the genealogical method. In this volume, the evolution of the Tonghua pharmaceutical firm organization, the formation of local entrepreneurship, historical accumulation of knowledge, and particular knowledge of transfer among generations of firms will be discussed, then I will probe into co-adaption and co-evolution between local formal and informal institutions and organizations in Tonghua’s TCM industry. In addition, I will try to understand the co-evolutionary process at different geographical levels (namely, national and local). In summary, my main findings include the following several points. Firstly, in the course of the emergence of Tonghua’s pharmaceutical industry, local social networks and the traditional alliance between enterprises and government have played important roles. Secondly, the most important factor that influences the evolution of endogenous industrial clusters such as the Tonghua pharmaceutical industry in transitional countries is not the change in technology, but the change in fundamental national institutions. Thirdly, the success of the Tonghua pharmaceutical industry can be ascribed to the creation of multiple paths largely based on initial conditions, which implies that economic policy should have historical consciousness, namely, new economic innovation should make full use of both historical legacies and existing assets. Finally, it is co-adaption and co-selection of firm organization, institution, and technology that have jointly made Tonghua’s pharmaceutical industry become highly competitive, which means that whether one region can grasp new opportunities partially depends on its capabilities to coordinate a varity of development agents.
Atmospheric observation-based global SF6 emissions - comparison of top-down and bottom-up estimates
(2009)
Emissions of sulphur hexafluoride (SF6), one of the strongest greenhouse gases on a per molecule basis, are targeted to be collectively reduced under the Kyoto Protocol. Because of its long atmospheric lifetime (≈3000 years), the accumulation of SF6 in the atmosphere is a direct measure of its global emissions. Examination of our extended data set of globally distributed high-precision SF6 observations shows an increase in SF6 abundance from near zero in the 1970s to a global mean of 6.7 ppt by the end of 2008. In-depth evaluation of our long-term data records shows that the global source of SF6 decreased after 1995, most likely due to SF6 emission reductions in industrialised countries, but increased again after 1998. By subtracting those emissions reported by Annex I countries to the United Nations Framework Convention of Climatic Change (UNFCCC) from our observation-inferred SF6 source leaves a surprisingly large gap of more than 70–80% of non-reported SF6 emissions in the last decade.
Fractional release factors of long-lived halogenated organic compounds in the tropical stratosphere
(2009)
Fractional release factors (FRFs) of organic trace gases are time-independent quantities that influence the calculation of Global Warming Potentials and Ozone Depletion Potentials. We present the first set of vertically resolved FRFs for 15 long-lived halo carbons in the tropical stratosphere up to 34 km altitude. They were calculated from measurements on air samples collected on board balloons and a high altitude aircraft. We compare the derived dependencies of FRFs on the mean stratospheric transit times (the so-called mean ages of air) with similarly derived FRFs originating from measurements at higher latitudes and find significant differences. Moreover a comparison with averaged FRFs currently used by the World Meteorological Organisation revealed the latter to be imprecise measures due to their observed vertical and latitudinal variability. The presented data set could thus be used to improve future ozone level and climate projections.
In this paper, similarity hypotheses for the atmospheric surface layer (ASL) are reviewed using nondimensional characteristic invariants, referred to as π -numbers. The basic idea of this dimensional π-invariants analysis (sometimes also called Buckingham’s π-theorem) is described in a mathematically generalized formalism. To illustrate the task of this powerful method and how it can be applied to deduce a variety of reasonable solutions by the formalized procedure of non-dimensionalization, various instances are represented that are relevant to the turbulence transfer across the ASL and prevailing structure of ASL turbulence. Within the framework of our review we consider both (a) Monin-Obukhov scaling for forced-convective conditions, and (b) Prandtl-Obukhov-Priestley scaling for free-convective conditions.It is shown that in the various instances of Monin-Obukhov scaling generally two π-numbers occur that result in corresponding similarity functions. In contrast to that, Prandtl-Obukhov-Priestley scaling will lead to only one π number in each case usually considered as a non-dimensional universal constant. Since an explicit mathematical relationship for the similarity functions cannot be obtained from a dimensional π-invariants analysis, elementary laws of π-invariants have to be pointed out using empirical or/and theoretical findings. To evaluate empirical similarity functions usually considered within the framework flux-profile relationships, so-called integral similarity functions for momentum and sensible heat are presented and assessed on the basis of the friction velocity and the vertical component of the eddy flux densities of sensible and latent heat directly measured during the GREIV I 1974 field campaign.
wo different single particle mass spectrometers were operated in parallel at the Swiss High Alpine Research Station Jungfraujoch (JFJ, 3580 m a.s.l.) during the Cloud and Aerosol Characterization Experiment (CLACE 6) in February and March 2007. During mixed phase cloud events ice crystals from 5 μm up to 20 μm were separated from large ice aggregates, non-activated, interstitial aerosol particles and supercooled droplets using an Ice-Counterflow Virtual Impactor (Ice-CVI). During one cloud period supercooled droplets were additionally sampled and analyzed by changing the Ice-CVI setup. The small ice particles and droplets were evaporated by injection into dry air inside the Ice-CVI. The resulting ice and droplet residues (IR and DR) were analyzed for size and composition by two single particle mass spectrometers: a custom-built Single Particle Laser-Ablation Time-of-Flight Mass Spectrometer (SPLAT) and a commercial Aerosol Time of Flight Mass Spectrometer (ATOFMS, TSI Model 3800). During CLACE 6 the SPLAT instrument characterized 355 individual ice residues that produced a mass spectrum for at least one polarity and the ATOFMS measured 152 particles. The mass spectra were binned in classes, based on the combination of dominating substances, such as mineral dust, sulfate, potassium and elemental carbon or organic material. The derived chemical information from the ice residues is compared to the JFJ ambient aerosol that was sampled while the measurement station was out of clouds (several thousand particles analyzed by SPLAT and ATOFMS) and to the composition of the residues of supercooled cloud droplets (SPLAT: 162 cloud droplet residues analyzed, ATOFMS: 1094). The measurements showed that mineral dust particles were strongly enhanced in the ice particle residues. 57% of the SPLAT spectra from ice residues were dominated by signatures from mineral compounds, and 78% of the ATOFMS spectra. Sulfate and nitrate containing particles were strongly depleted in the ice residues. Sulfate was found to dominate the droplet residues (~90% of the particles). The results from the two different single particle mass spectrometers were generally in agreement. Differences in the results originate from several causes, such as the different wavelength of the desorption and ionisation lasers and different size-dependent particle detection efficiencies.