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Pessel M. & Gibert D. (2003). Multiscale electrical impedance tomography. J. Geophys. Res., 108(b1).
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Lambert J.-c., Balis D., Goutail F., Granville J., Hubert D., Keppens A., Koukouli M., Laeng A., Pommereau J.-p., Rahpoe N., Sofieva V. Et Al. (2015). CCI-Ozone Fundamental Climate Data Records: Evaluation of compliance with GCOS requirements and research needs.
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Lerot C., Danckaert T., Van Roozendael M., Spurr R., Loyola D., Coldewey-egbers M., Koukouli M., Balis D., Zyrichidou I., Lambert J.-c., Granville J. Et Al. (2015). Extension of the ESA CCI Total Ozone Climate Data Record with the Application of the GODFITv3 Algorithm to OMI Observations.
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Chattová Barbora, Lebouvier Marc, Van de Vijver Bart. (2014). Freshwater diatom communities from Ile Amsterdam (TAAF, southern Indian Ocean)
. FOTTEA, 14(article_1), 101–119.
Keywords: Bacillariophyta; biogeography; ecology; Ile Amsterdam; southern Indian Ocean; sub-Antarctic region,
Programme: 136
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Xavier José, Clarke M R, Magalhães M C, Stowasser G, Blanco C, Cherel Y, . (2007). Current status of using beaks to identify cephalopods : III International Workshop and training course on Cephalopod beaks , Faial island , Azores , April 2007
(Vol. 24).
Abstract: The identification of cephalopods using their beaks is still a difficult technique. To increase our knowledge of this technique and stimulate a new generation of beak experts, the III International beak workshop and training course was organized in Faial, Azores Islands in 2007. We briefly review the activities of the workshop, including the identification procedure of lower beaks of cephalopods from predators with emphasis on cetaceans, seals, fish and seabirds; provision of basic knowledge to young researchers interested in the study area; identification of recent developments in beak research; and discussion of the main problematic issues. The families that need particular attention are Brachioteuthidae, Chiroteuthidae, Cranchiidae, Cycloteuthidae, Mastigoteuthidae, Octopoteuthidae, Promachoteuthidae, Onychoteuthidae (particularly the genus Walvisteuthis), Mastigoteuthidae and Cirroteuthidae. The stable isotopic signature of beaks is capable of revealing new trophic relationships and migrations. Future work should focus on: a) obtaining more cephalopod material from research cruises; b) promoting a close and continuous collaboration between beak experts and cephalopod taxonomists and; c) developing new, and updated, beak guides.
Keywords: 18, campus de gambelas, cantab, ccmar, centro de ciências do, clarke, collections, e mail, erosion, fcma, jccx, josé xavier, malcolm r, mar do algarve, museum, net, portugal, pt, pt 8005 139 faro, rua do porto, são joão, species, sperm whale squid, taxonomy, trophic relationships, universidade do algarve,
Programme: 109
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Andre R., Villain J.P., Krassnosel'skikh V. & Hanuise C. (2000). Super dual aurora radar network observations of velocity-divergent structures in the F region ionosphere. J. Geophys. Res., 105(a9), 20899–20908.
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Chisham G, Freeman M P, Abel G A, Bristow W A, Marchaudon A, Ruohoniemi J M, Sofko G J, . (2009). Spatial distribution of average vorticity in the high-latitude ionosphere and its variation with interplanetary magnetic field direction and season
. J. Geophys. Res., 114(A9), A09301–.
Abstract: We present a technique to measure the magnetic field-aligned vorticity of mesoscale plasma flows in the F region ionosphere using line-of-sight velocity measurements made by the Super Dual Auroral Radar Network (SuperDARN). Vorticity is often used as a proxy for magnetic field-aligned current (FAC) intensity in the ionosphere but also provides information about turbulent processes in the ionosphere and magnetosphere. Using 6 years (2000–2005 inclusive) of vorticity measurements made by six SuperDARN radars in the Northern Hemisphere, we have compiled, for the first time, maps of average vorticity across the northern polar ionosphere. These maps have been subdivided according to different seasonal and interplanetary magnetic field (IMF) conditions. The variations in the morphology of the vorticity maps with IMF direction match very closely those seen in maps of average FAC intensity (determined using different methods and instrumentation), suggesting that vorticity is a good proxy for FAC in an averaged sense. The variations in the morphology of the vorticity maps with season show differences from those seen in the FAC maps, illustrating that ionospheric conductance plays a major role in determining the differences between measurements of vorticity and FAC.
Keywords: ionosphere, vorticity, field-aligned current, 2431 Ionosphere: Ionosphere/magnetosphere interactions, 2409 Ionosphere: Current systems, 2437 Ionosphere: Ionospheric dynamics, 2494 Ionosphere: Instruments and techniques, 2721 Magnetospheric Physics: Field-aligned currents and current systems,
Programme: 312;911
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Prikryl P., Greenwald R.A., Sofko G.J., Villain J.P., Ziesolleck C.W.S. & Friis Christensen E. (1998). Solar-wind-driven pulsed magnetic reconnection at the dayside magnetopause, Pc5 compressional oscillations, and field line resonances. J. Geophys. Res., 103(a8), 17307–17322.
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Watanabe M., Pinnock M., Rodger A.S., Sato N., Yamagishi H., Yukimatu A.S., Greenwald R.A., Villain J.P. & Hairston M.R. (1998). Localized activation of the distant tail neutral line just prior to substorm onsets. J. Geophys. Res., 103(a8), 17651–17669.
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Huang C.S., Sofko G.J., Koustov A.V., Mcdougall J.W., Greenwald R.A., Ruohoniemi J.M., Villain J.P., Lester M., . & a.l. (2001). Long-period magnetospheric-ionospheric perturbations during northward interplanetary magnetic field. J. Geophys. Res., 106(a7), 13091–13103.
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