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Displaying: 101 - 120 of 196 Next
101. ENVISAT AO - ID:158: CINAMON: Characterisation, INterpretation, Application, and Maturation of key Ozone-related ENVISAT-1 level-2 products, using correlative observations associated with the NDSC

The present project aims at the geophysical validation, from pole to pole and on the long term, of key ozone-related level-2 products (O3, NO2, BrO, OClO, and ClO) from GOMOS, MIPAS and SCIAMACHY onboard ENVISAT-1, and at a contribution to the maturation of the related level-1b-to-2 data processors. Application data processing will be used to convert level-2 data into a more suitable format for validation and scientific end-users. The respective performances of the ENVISAT data products, and their sensitivity to various relevant parameters, will be investigated from the Arctic to the Antarctic, over a variety of geophysical conditions. The impact of these performances on specific atmospheric chemistry studies will be emphasised. The pseudo-global investigations will rely on correlative studies of ENVISAT data with high-quality ground-based, in situ and balloon observations associated with the Network for the Detection of Stratospheric Change (NDSC).

Atmospheric processes Sources Ozone Climate variability NDSC Spatial trends Pollution sources Climate change Emissions Atmosphere Temporal trends satellite validation
102. ENVISAT AO - ID:126: Validation of ENVISAT-1 level-2 products related to lower atmosphere O3 and NOy chemistry by an FTIR

The project will provide a long-term, pseudo-global validation support to the ENVISAT-1 atmospheric measurements, based on mutually consistent high-quality solar and lunar observations from FTIR spectrometers operated at primary and a number of complementary NDSC stations. The validation is limited to a number of target species, most of which are primary NRT or OL level-2 products of the mission, with focus on NOy components: O3, NO2, NO, N2O, HNO3, HNO4, H2CO, CO and CH4. Synergistic use will be made of column and profile data from MIPAS, GOMOS and SCIAMACHY. The ground network will deliver mean vertical column abundances for all target species with NDSC-type quality, and height profile information for some target gases as secondary products to the PI's home institute, where the correlative analyses with the ENVISAT-1 products will be done. Asynoptic mapping tools will support the validation efforts.

Atmospheric processes Sources Ozone FTIR Mapping Climate variability NDSC Spatial trends Pollution sources Climate change Emissions Atmosphere Temporal trends satellite validation
103. Radiometric studies of natural surfaces at Ny-Aalesund by means of field survey and multispectral satellite data

The main goal of this research project is to complete the collection of snow/ice field data and to improve the organization of snow/ice spectral signatures, and structural data, along with ancillary information in the existing archive.

Geology Mapping radiometric studies remote-sensing Spatial trends Climate change Ice Arctic Temporal trends spectral reflectance
104. ESAC I and II: Experimental Studies of Atmospheric Changes, 1st and 2nd phase

The main objectives of ESAC II are the following: (1) Extend and improve the important existing Belgian contribution in atmospheric research started in the 50s, recognized internationally. (2) Investigate the chemistry of the atmosphere, to detect and understand its evolution, mainly with experimental means. Special attention will be paid to the evolution of the ozone layer and chemical species and processes with an impact on climate changes. (3) Support the Belgian policies and decisions regarding the Amendments to: - the Montreal Protocol on Substances that deplete the Ozone Layer; - the Kyoto Protocol on Greenhouse Gases (GHG) emissions.

Atmospheric processes Sources Ozone UV radiation Climate variability Belgian contribution in atmospheric research Spatial trends Pollution sources Montreal & Kyoto Protocols Climate change Modelling Emissions Atmosphere Temporal trends
105. Greenland Arctic Shelf Ice and Climate Experiment

-Quantify changes in ice dynamics and characteristics resulting from the switch in AO phase -Establish a climate record for the region north of Greenland through the retrieval and analysis of sediment cores -Improve an existing dynamic-thermodynamic sea ice model, focusing on the heavily deformed ice common in the region -Relate the region-specific changes which have occurred to the larger-scale Arctic variablity pattern -Place the recent ice and climate variability for this critical region into the context of long term climate record, as reconstructed from sediment cores

Climate variability Climate Sea ice Environmental management Climate change Modelling Ice Arctic Ice cores Temporal trends
106. EARLINET: A European Aerosol Research Lidar Network to Establish an Aerosol Climatology

EARLINET will establish a quantitative comprehensive statistical database of the horizontal, vertical, and temporal distribution of aerosols on a continental scale. The goal is to provide aerosol data with unbiased sampling, for important selected processes, and air-mass history, together with comprehensive analyses of these data. The objectives will be reached by implementing a network of 21 stations distributed over most of Europe, using advanced quantitative laser remote sensing to directly measure the vertical distribution of aerosols, supported by a suite of more conventional observations. Special care will be taken to assure data quality, including intercomparisons at instrument and evaluation levels. A major part of the measurements will be performed according to a fixed schedule to provide an unbiased statistically significant data set. Additional measurements will be performed to specifically address important processes that are localised either in space or time. Back-trajectories derived from operational weather prediction models will be used to characterise the history of the observed air parcels, accounting explicitly for the vertical distribution.

Atmospheric processes Climate variability Spatial trends Climate change Data management Atmosphere Temporal trends
107. SOGE: System for Observation of halogenated Greenhouse gases in Europe

SOGE is an integrated system for observation of halogenated greenhouse gases in Europe. There are two objectives: (1) To develop a new cost-effective long-term European observation system for halocarbons. The results will be in support of the Kyoto and the Montreal protocols,in assessing the compliance of European regions with the protocol requirements. In particular the observation system will be set up to: - detect trends in the concentrations of greenhouse active and ozone-destroying halocarbons; - verify reported emissions and validate emission inventories; - develop observational capacity for all halocarbons included in the Kyoto protocol (PFC, SF6) for which this is presently not yet existing; - develop a strategy for a cost-effective long-term observation system for halocarbons in Europe. (2) To predict and assess impacts of the halocarbons on the climate and on the ozone layer. This implies extensive exploitation of existing data. The impact assessment will be aimed at providing guidance for development of the Kyoto protocol and to the further development of the Montreal protocol mendments, by: - modelling impacts of halocarbons on radiative forcing and their relative importance for climate change; - modelling impacts of emissions of CFCs and HCFCs on the ozone layer.

Atmospheric processes Sources Ozone Climate variability Spatial trends Pollution sources Climate change Modelling Emissions Atmosphere Temporal trends
108. QUILT: Quantification and Interpretation of Long-Term UV-Vis Observations of the Stratosphere

The aim of QUILT is to optimise the exploitation of the existing European UV-visible monitoring systems by which O3 and the related free radicals NO2, BrO and OClO can be measured. These monitoring systems include ground-based, balloon and satellite observations. QUILT is providing an assessment of the chemical ozone loss over the last decade and through 2000-2003. This is achieved through analysis improvements, consolidation of existing datasets and near real time integrations with chemical transport models.

Atmospheric processes Sources Ozone Stratospheric Ozone Montreal Protocol Climate variability Spatial trends Pollution sources UV-Visible Remote Sensing Climate change Modelling Emissions Atmosphere Temporal trends Satellite Validation
109. FREETEX (part of TROTREP): The Free troposphere experiment

The goals of this experiment are to map out the chemical changes in the free troposphere as the atmosphere transitions from winter to spring. It is hoped to begin to understand the chemical conditions that influence the lifetime of ozone and understand more about the productivity of this region of the atmosphere with respect to the in-situ production of ozone. How the free troposphere responds to changing levels of pollution could be critical to the development of future abatement strategies.

Atmospheric processes Sources Ozone Mapping Climate variability Pollution sources Climate change Emissions Atmosphere
110. COSE: Compilation of atmospheric Observations in support of Satellite measurements over Europe

The overall objective of COSE is to provide the Earth Observation (EO) user community with a validated, consistent and well-documented data set of mainly stratospheric constituent columns and/or profiles, by co-ordination of ground-based observations at existing stations in Europe. The data set builds on past and ongoing time series, and will be archived in a dedicated database for immediate and future exploitation, e.g., satellite validation activities, data assimilation and scientific studies. Active participation of some representative EO customers will assure that the delivered data sets come up to their requirements.

Atmospheric processes Sources Ozone network observations database Climate variability Atmospheric chemistry monitoring Spatial trends Pollution sources Climate change Modelling Emissions data documentation and user exploitation Data management Atmosphere Temporal trends satellite validation
111. Global Climate Change, Faunal Invasion And Succession In High arctic Ecosystems : Implications For Ecosystem Function.

Prof. I.D. Hodkinson Dr. S.J. Coulson School of Biological & Earth Sciences, Liverpool John Moores University, Byrom St., Liverpool L3 3AF, UK (Contact details: Tel. 0151 2312030 Fax. 0151 207 3224 email; Prof. N.R. Webb NERC Centre for Ecology & Hydrology, Winfrith Technology Centre, Dorchester, Dorset, DT2 8ZD, (Contact details: email Objectives and Hypotheses Our main objectives are to:  describe, measure and model patterns and rates of invertebrate community development and succession following glacial retreat in the high Arctic using known chronosequences.  cross-relate rates of community change to known climatic shifts.  relate invertebrate community development to rates of key ecological processes such as decomposition of organic matter.  evaluate the potential for more southerly species successfully to invade existing Arctic invertebrate communities.  develop descriptive and predictive models of community development under conditions of climatic amelioration. We are testing the following hypotheses:  that dispersal of particular functional groups of invertebrates in response to climate warming is a rate-limiting factor for invertebrate succession and community development in the high Arctic.  that invertebrate community development in response to climatic warming is deterministic and directional, and therefore predictable.  that the magnitude and stability of key ecosystem processes, such as decomposition, in the high Arctic are linked to biotic complexity, which can be suitably characterised by the invertebrate community composition.  that natural succession provides a useful model for predicting rates of invasion by colonising species following climatic amelioration. Study sites Studies on two contrasting but complementary chronosequences on west Spitsbergen commenced in June 2000, an oligotrophic succession on t he glacial foreland of Midtre Lovénbre and a relatively eutrophic succession on Lovénøyene, a series of islands in Kongsfjord. A 1.5 km transect was established, extending from the foot of the Midtre Lovénbre to the terminal moraines and across the sandur. Seven equally spaced sampling sites (approx 20 x 40 m) were established at right angles to the main transect line). Each site was chosen to represent the most mature vegetation type present at each point. By contrast, each Lovénøy was viewed as a separate sample site. The chronology of glacial 'retreat' was established from vertical and oblique aerial and ground based photographs held by the Norsk Polarinstitutt Archive, Tromsø, from historical records and ground photographs and, for the oldest site, by radiocarbon dating of the soil. Results Ages of sites: The ages of the sites from the Midtre Lovénbre sequence vary between 2 years (site one) to 1900 (site seven), while the islands vary between 100 (Leirholmen) to 1800 (Storholmen). Plant community description and soil formation A detailed description has been made in the changes in the plant community (18 taxa) from site 1-7 on the Lovénbre - from unconsolidated parent to almost 100% ground cover. The presence, abundance and dynamics of each species have been described. Species have been characterised as early, mid or late successional. Parallel trends occur in soil characteristics including increasing depth, increasing organic matter and water content, decreasing clast size and a lowering of pH. Animal community description The soil fauna comprise primarily Collembola, mites, Enchytraeidae and chironomid larvae. Herbivores (one aphid and sawfly larvae) are few but hymenopteran parasitoids and predators (spiders and gamasid mites) are abundant. The distribution patterns of species and their abundances have been quantified for both the Lovénbre and Lovénøyene chronosequnces. The very first colonisers of bare moraines are Linyphiid spider species (predators). Other early soil colonisers are generally the surface active species such as the collembolan Isotoma anglicana. The poorest colonisers are the deep soil dwelling species. Experiments are thus underway examining wind blown dispersal and survival on seawater. A cellular automaton model, using absolute density and pitfall trap is being used to simulate diffusion dispersal of soil animals. A set of unusual weather conditions in late July produced a mass immigration of a small moth Plutella xylostella into Svalbard. This chance event has allowed us to track in detail the movement of associated weather systems and to reconstruct the direction and source of immigrants. Such events are rare but may become increasingly frequent as climate changes, opening a closed gateway for animals from further south to move into the Arctic. Continuing work Current visit (late July/early August) is aimed at collecting supporting information on the plant cover and microhabitat characteristics for manuscripts in preparation.

Climate change
112. UFTIR: Time Series of Upper Free Troposphere observations from a European ground-based FTIR network

The main specific objectives of UFTIR are: (1) To revise and homogenise the analyses of available experimental data for providing consistent time series of distinct tropospheric and stratospheric abundances of the target gases using new inversion algorithms. A common strategy for retrieval and characterisation of the vertical distributions of the target gases from FTIR ground-based measurements will be established. (2) To provide quantitative trends and associated uncertainties for the target gases over about the last decade, as a function of latitude throughout Western Europe, focusing on the troposphere. (3) To integrate the data in model assessments of the evolutions of tropospheric abundances. The measured burden and changes of the tropospheric gases will be compared with 3D model simulations, in order to help developing the latter, assist in explaining potential causes for the observed changes and to assess the consistencies between the trends at the surface to the free troposphere and lowermost stratosphere, and the agreement with known evolutions of emissions. UFTIR will make the community prepared to deliver tropospheric data for validation and synergistic exploitation of new satellite experiments like ENVISAT.

Atmospheric processes Sources Ozone FTIR Climate variability Spatial trends Pollution sources Climate change Modelling Emissions Atmosphere Temporal trends profile inversions
113. Climate Change and Competitive Interactions

The effects of climate change in a dynamic competitive interaction between two or more species can be bought about either as direct responses of species to change or indirectly through effects on competing species. Intertidal barnacles are ideal model organisms to test these alternative causal mechanisms, being easily censussed and directly competing for space. Single- and multi- species models will be developed for barnacles in SW England to determine whether direct or indirect mechanisms better predict responses to change. The models will include functions for space-limitation, environmental influence and, in the latter models, functions for interspecific competition. Historical data from a network of sites collected over a 40-year period will be used to develop and test the models.

Climate variability Spatial trends Climate change Biodiversity Temporal trends Ecosystems
114. Long-Term and Solar Variability effects in the Upper Atmosphere

Objective: to determine how solar activity influences temperatures, winds, electric currents and minor constituents and to allow possible anthropogenic influences to be determined. Uses primarily measurements by the ESRAD and EISCAT radars, plus ground-based and balloon-borne measurements of atmospheric electric fields and currents.

Atmospheric processes Noctilucent clouds Geophysics Climate variability Solar Proton Events Climate Climate change Modelling Emissions Arctic Atmosphere Polar mesospheric summer echoes (PMSE) Temporal trends
115. PINE

PINE (Predicting Impacts on Natural Ecotones) will investigate the potential impacts of key land-use management decisions on the European tree-line ecotones under different climatic change scenarios. The focus is on identifying critical thresholds of change, some of which may be irreversible. The aim is to inform decision makers of the consequences of their actions in terms of sustainable development, landscape change and biodiversity. The first step will be to assess the decision-makers’ and stakeholders’ perceptions of environmental change and risk. We will then go on to produce a spatially explicit, dynamic forest succession model (TreeMig) tuned specifically to tree-line ecotones. The model parameters are defined using variables which initiate, control and terminate tree growth. These are derived from cambium dynamics and an innovative multi-proxy approach in which the proxies used are tree ring width, density, stable carbon isotope ratios, height increment, needle production and pollen deposition. Data will be collected from a range of tree-line tree species at sites in Sweden, Finland, Austria, Italy and Slovenia. The model will be evaluated using the past response of tree line plant communities to climatic change under varying management regimes and then used to predict changes in the tree-line ecotones in response to climatic change under different land-use change scenarios.


Detailed inventory of four peaks at altitudes ; just above subalpine, between low alpine and middle alpine, between middle alpine and high alpine and at highalpine. Vegetation cover and plant species with abundance are inventored with different methods. Temperature loggers are burried in main geographical directions. The purpose is to reinventory these peaks after a longer period (about 5 to 10 years) and analyse eventual differences. The project is coorinated by the University of Wien in Austria. The peaks inventoried is west of Tornehamn, south and east of Latnjajaure and Kårsatjåkka.

117. Debris mobilisation and transfer within periglacial catchments, Abisko mountains, Sweden

The purpose of the project is to study the geomorphological processes that accomplish sediment transfers in mountain catchments in the Abisko area. Using both field data and remote sensing methods, an attempt will be made to model the processes and the resulting effects on landforms within a GIS. Methods of estimating process frequency or rate, e.g. by lichenometry, will be used. Main field site is the Nissunvagge valley, previously studied in the 1980´s (Nyberg 1985). The results will be evaluated from a climate change perspective.

118. Stratosphere-mesosphere intercomparison of ozone profil

During the past years, atmospheric research in high latitudes has been focussed on processes causing ozone loss in the polar winter lower stratosphere1). Recent research efforts also dealt with regions up to the lower mesosphere, and studied the effects of charged particle precipitation on NO and ozone2)-5). However, the measurement techniques and hence the database for studying such processes in this altitude range are very limited. The Airborne SUbmillimeter Radiometer ASUR6),7) of the Institute of Environmental Physics of the University of Bremen has recently been equipped with a high-resolution spectrometer that will enable the retrieval of vertical profiles of ozone up to an altitude of about 65 - 70 km. Its measurement capabilities comprise also several other species of interest, especially NO. This makes the measurement technique particularly suitable for upper stratospheric/lower mesospheric studies. The lidar at ALOMAR is capable of measuring highly resolved vertical profiles of ozone up to an altitude of 60 km, thus giving the rare opportunity for intercomparison and validation studies in an altitude range reaching from the lower stratosphere to the lower mesosphere. Therefore we propose to perform simultaneous ozone measurements of the ASUR instrument with the ALOMAR lidar, supported by launches of ozone sondes.

Atmospheric processes Ozone Geophysics radiometer Climate Arctic Atmosphere lidar
119. Ground-based observations of noctilucent clouds With the shortest possible wavelength (308 nm)

Noctilucent clouds (NLC) remain a fascinating phenomenon of the upper atmosphere to study. The questions about the typical particle density and particle size distribution within a NLC are very prominent ones, to which a number of answers have been given, though some of the answers contradict each other. The parameters of particle size distributions can be derived from groundbased lidar measurements of the spectral dependence of the volume backscatter coefficient of an NLC. Such studies have been performed during a number of NLC events by e.g. the ALOMAR Rayleigh/Mie/Raman (RMR) lidar (von Cossart et al., GRL, 26, 1513, 1999). A drawback of these experiments is the wavelength limitation of the RMR lidar, the shortest wavelength of which is 355 nm. At this wavelength, the sensitivity of the lidar to particles with sizes smaller than, say, 25 nm is minimal. Because a considerable part of the entire particle population may have sizes below that threshold, a lingering question remains whether or not this drawback matters for typical NLC distributions. Using the ALOMAR ozone lidar, a measurement of the NLC volume backscatter coefficient at 308 nm becomes possible. Due to the l-4 -dependence of the backscatter coefficients, the latter are almost a factor of 2 larger at this wavelength than at 355 nm. For this reason and in order to gain a fourth wavelength to the spectral distribution, we aim at using the ozone lidar for the outlined project.

Atmospheric processes Climate NLC Arctic Atmosphere lidar
120. Study of the ozone response to the winter-spring time atmospheric dynamics at high latitude

These investigations confirm the fact that in the stratosphere the ozone is considerably influenced by dynamical processes and it is a good indicator of them. In this context the main objectives of the proposed study are: 1) to investigate the possible relationship between stratospheric ozone perturbations and the temperature enhancement in the upper mesosphere, observed by Shepherd et al. (2001); 2) to examine whether changes in ozone, concomitant with the phenomenon, take place and how and when they would be manifested; and 3) to investigate the stratospheric ozone behaviour during the equinox atmospheric transition in the North Hemisphere, for better understanding of the middle atmosphere dynamics.

Ozone Geophysics stratospheric warming Climate Arctic Atmosphere polar vortex