ALBERT

Description: Final Report, EU Concerted Action Introductions with Ships (MAS3-CT97-0111): Until recently, the importance of ballast water as a major transfer vector that affect aquatic ecosystem stability and modify biodiversity was not generally recognised, although studies on species transfer via ballast water in maritime countries have increased world-wide. Despite considerable research effort (national and international), there has been virtually no consideration of the effectiveness or standardisation of ballast water sampling methodology in order to monitor effectiveness of control measures. One key objective of the Concerted Action was to test monitoring systems for sampling ballast water. Two major intercalibration workshops compared sampling techniques. The largely varying conditions onboard ships require to develop a “tool box” rather than singling out one method, thereby combining qualitative and quantitative sample analysis for plankton species composition and abundance. The two intercalibration workshops delivered results allowing better comparisons of ship sampling studies around the world. The second key issue was to gain more insight on species composition in ballast water during ship voyages. This was achieved by ocean-going workshops (OGWs). The data obtained during five OGWs, using the “tool box” originated from European voyages (three OGWs) and during inter-ocean voyages (two OGWs). In total, approximately 700 samples were collected during more than 100 days at sea. More species and specimens were found in new ballast water, and communities were in general similar to outside seawater where ballasting took place. The highest number of phytoplankton species found was 52, including potentially toxic species. At most, 40 zooplankton taxa were found. Abundance and diversity of phyto- and zooplankton species remained fairly stable for 3-4 days, followed by an exponential decline. In some cases no living zooplankton were found after 9 days, in others about 10% of the taxa survived, remaining viable for 25 days (i.e. voyage Hong Kong – Hamburg). Sampling showed that in calm conditions phytoplankton exhibited a vertical zonation in ballast tanks. During rough weather mixing occurred causing increasing in mortality. For the first time in ballast water studies, traps were used with bait and light as attractants, catching taxa not seen in the net samples before. The effect of mid ocean exchange (MOE), recommended by International Maritime Organization (IMO) as a measure against unintentional introduction via ships, was studied. In many cases the number of taxa increased rather than declined while densities of specimens were diluted. A public awareness was launched, preparing a video, a leaflet, flyers, press releases, newsletter articles of International Aquatic Societies, an Internet homepage (visit the homepage at: http://members.aol.com/sgollasch/sgollasch/index.htm *) and several posters. A book on case histories, listing species previously introduced to European waters, was prepared especially to address harbour and regulatory authorities. Assessment of potential control measures (treatment) to reduce risks arising from ballast water releases included the evaluation and development of guidelines for ballast water treatment options. All participants provided input on references (e.g. grey literature, governmental reports, internal reports from harbour authorities, interim project reports) into a database kept by the co-ordinator. The Concerted Action reviewed and considered shipping studies both within and outside the EU. This provided a more balanced view of the state of the art and also enabled the Intercalibration workshops to consider and compare sampling methods as used throughout the world. During the CA many of these studies were completed and new ones studies commenced. It is recommended that the EU takes advantage of the well developed expertise within the network of the CA partners to gain momentum in an area where global solutions are urgently needed.

Description: Scientists planning to use underwater stereoscopic image technologies are often faced with numerous problems during the methodological implementations: commercial equipment is too expensive; the setup or calibration is too complex; or the imaging processing (i.e. measuring objects in the stereo-images) is too complicated to be performed without a time-consuming phase of training and evaluation. The present paper addresses some of these problems and describes a workflow for stereoscopic measurements for marine biologists. It also provides instructions on how to assemble an underwater stereo-photographic system with two digital consumer cameras and gives step-by-step guidelines for setting up the hardware. The second part details a software procedure to correct stereo-image pairs for lens distortions, which is especially important when using cameras with non-calibrated optical units. The final part presents a guide to the process of measuring the lengths (or distances) of objects in stereoscopic image pairs. To reveal the applicability and the restrictions of the described systems and to test the effects of different types of camera (a compact camera and an SLR type), experiments were performed to determine the precision and accuracy of two generic stereo-imaging units: a diver-operated system based on two Olympus Mju 1030SW compact cameras and a cable-connected observatory system based on two Canon 1100D SLR cameras. In the simplest setup without any correction for lens distortion, the low-budget Olympus Mju 1030SW system achieved mean accuracy errors (percentage deviation of a measurement from the object’s real size) between 10.2 and –7.6% (overall mean value: –0.6%), depending on the size, orientation and distance of the measured object from the camera. With the single lens reflex (SLR) system, very similar values between 10.1% and –3.4% (overall mean value: –1.2%) were observed. Correction of the lens distortion significantly improved the mean accuracy errors of either system. Even more, system precision (spread of the accuracy) improved significantly in both systems. Neither the use of a wide-angle converter nor multiple reassembly of the system had a significant negative effect on the results. The study shows that underwater stereophotography, independent of the system, has a high potential for robust and non-destructive in situ sampling and can be used without prior specialist training.

Description: Digital Elevation Models (DEMs) of flat lowlying coastlands are becoming even more important for environmental risk analyses, for example the development of effective plans for flooding protection. The need of information at high spatial resolution over very large areas, of the order of 100×100 km2, practically precludes the use of traditional methods (e.g., leveling and DGPS) due to their intrinsic limitation in covering wide zones and reduces the possibility of using Lidar because of its high cost. Starting from the last decade, space-borne radar sensors have been used extensively for this purpose. The most known is the SRTM (Shuttle Radar Topographic Mission) DEM which covers most of the land area between ±60° latitude. This DEM was generated using singlepass interferometry and is widely available at 3-arc-seconds. In this work, we present the results obtained for the Veneto plain, Italy, using the spaceborne SAR (Synthetic Aperture Radar) crossinterferometry.

Description: Published

Description: Bologna, Italy

Description: 5IT. Osservazioni satellitari

Description: open

Description: This is the first volume of the entirely rewritten, revised and updated version of the original FAO Catalogue of Cephalopods of the World (1984). The present Volume is a multiauthored compilation that reviews six families: Nautilidae, Sepiidae, Sepiolidae, Sepiadariidae, Idiosepiidae and Spirulidae, with 23 genera and the 201 species known to the date of the completion of the volume. It provides accounts for all families and genera, as well as illustrated keys to all taxa. Information under each species account includes: valid modern systematic name and original citation of the species (or subspecies); main synonyms; English, French and Spanish FAO names for the species; illustrations of dorsal and ventral aspect of the whole animal (as necessary) and other distinguishing illustrations; field characteristics; diagnostic features; geographic and vertical distribution, including GIS map; size; habitat; biology; interest to fishery; local names when available; a remarks section (as necess ary) and literature. The volume is fully indexed and also includes sections on terminology and measurements, an extensive glossary, an introduction with an updated review of the existing biological knowledge on cephalopods (including fisheries information and catch data for recent years) and a dedicated bibliography.

Description: Models of sedimentary basins mostly regard the lithospheric mantle as a homogeneously dense body.Tomographic and seismological studies, in contrast, indicate lateral heterogeneities in the mantle. Several studiesaddressed these heterogeneities by inverting seismic wave velocity from tomographic models to tem-perature and density. Whilst these studies have shown that sensitivity of seismic velocity to variations in temperature is larger than to variations in density (e.g. Sobolev et al., 1996), the differentiation of thermal from compositional anomalies remains difficult. We aim to solve this problem by quantifying the impact of varying mantle compositions on inverted density dis-tributions and the calculated gravity field of the mantle above 300km depth. Therefore, we use forward calculation of s- and p-wave velocities to invert tomographic models for temperature and density, considering laboratory mineral properties and different mantle compositions (Goes et al., 2000). Thereby, we consider tomographic models on global and regional scale. Our results indicate a significant impact on the inferred gravity field and thus on interpretations of lithospheric-scale models. Furthermore, we find that the integration of inverted density distributions may decrease uncertainties in the interpretation of gravity-constrained basin models. Additionally, for models with well constrained upper lithospheric structure, i.e. from reflection and refraction seismics, the integration of inverted density distributions in the upper mantle may help to identify compositional or thermal anomalies in the mantle.

Description: Methane sources and sinks in the Arctic are poorly quantified. In particular, methane emissions from the Arctic Ocean and the potential sink capacity are still under debate. In this context sea ice impact on and the intense cycling of methane between sea ice and Polar surface water (PSW) becomes pivotal. We report on methane super- and under-saturation in PSW in the Eurasian Basin (EB), strongly linked to sea ice-ocean interactions. In the southern EB under-saturation in PSW is caused by both inflow of warm Atlantic water and short-time contact with sea ice. By comparison in the northern EB long-time sea ice-PSW contact triggered by freezing and melting events induces a methane excess. We reveal the Ttranspolar Drift Stream as crucial for methane transport and show that inter-annual shifts in sea ice drift patterns generate inter-annually patchy methane excess in PSW. Using backward trajectories combined with δ18O signatures of sea ice cores we determine the sea ice source regions to be in the Laptev Sea Polynyas and the off shelf regime in 2011 and 2015, respectively. We denote the Transpolar Drift regime as decisive for the fate of methane released on the Siberian shelves.

Description: Methane sources and sinks in the Arctic are poorly quantified. In particular, methane emissions from the Arctic Ocean and the potential sink capacity are still under debate. In this context sea ice impact on and the intense cycling of methane between sea ice and Polar surface water (PSW) becomes pivotal. We report on methane super- and under-saturation in PSW in the Eurasian Basin (EB), strongly linked to sea ice-ocean interactions. In the southern EB under-saturation in PSW is caused by both inflow of warm Atlantic water and short-time contact with sea ice. By comparison in the northern EB long-time sea ice-PSW contact triggered by freezing and melting events induces a methane excess. We reveal the Ttranspolar Drift Stream as crucial for methane transport and show that inter-annual shifts in sea ice drift patterns generate inter-annually patchy methane excess in PSW. Using backward trajectories combined with δ18O signatures of sea ice cores we determine the sea ice source regions to be in the Laptev Sea Polynyas and the off shelf regime in 2011 and 2015, respectively. We denote the Transpolar Drift regime as decisive for the fate of methane released on the Siberian shelves.