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Woehler E.J., Cooper J., Croxall J.P., Fraser W.R., Kooyman G.L., Miller G.D., Nel D.C., Patterson D.L., Peter H.U., Ribic C.A., Salwicka K., Trivelpiece W.Z. & Weimerskirch H. (2001). A statistical assessment of the status and trends of Antarctic and Subantarctic seabirds..
Abstract: Report on SCAR BBS Workshop on Southern Ocean seabird populations
43pages
Programme: 109
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Chisham G., Freeman M.P., Sotirelis T., Greenwald R.A., Lester M.L.E. & Villain J.-P. (2005). A statistical comparison of SuperDARN spectral width boundaries and DMSP particle precipitation boundaries in the morning sector ionosphere. Annales geophysicae, 23, 733–743.
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El-Lemdani Mazouz F., M. Menvielle, A. Chambodut, A. Marchaudon, C. Lathuillière. (2012). A statistical study of LT variations of aλ sectorial geomagnetic indices.
Abstract: XV IAGA Workshop On “Geomagnetic Observatory Instruments, Data Acquisition and Processing”, SanFernando, Espagne.
Programme: 905
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El-Lemdani Mazouz F., M. Menvielle, A. Chambodut, A. Marchaudon, C. Lathuillière . (2012). A statistical study of LT variations of aλ sectorial geomagnetic indices.
Abstract: XV IAGA Workshop On “Geomagnetic Observatory Instruments, Data Acquisition and Processing”, SanFernando, Espagne.
Programme: 139
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Villain J.P., André R., Pinnock M., Greenwald R.A. & Hanuise C. (2002). A statistical study of the Doppler spectral width of high-latitude F-region echoes recorded with SuperDARN coherent HF radars. Annales geophysicae, 20, 1769–1781.
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Fressin, F.; Guillot, T.; Schmider, F.-X.; Agabi, A.; Moutou, C.; Aigrain, S.; Bouchy, F.; Boer, M.; Pont, F.; Erikson, A.; Rauer, H.; The A Step Team. (2007). A STEP: Towards a Large Photometric Survey for Exoplanets at Dome C (Vol. 25).
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Grannas A.M., Shepson P.B., Guimbaud C., Albert M., Simpson W., Dominé F., Boudries H. (2002). A Study of Carbonyl Compounds and Photochemistry in the Arctic Atmospheric Boundary Layer. Atmospheric environment, 36, 2733–2742.
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Steelandt Stéphanie, Marguerie Dominique, Bhiry Najat, Delwaide Ann, . (2015). A study of the composition, characteristics, and origin of modern driftwood on the western coast of Nunavik (Quebec, Canada)
. J. Geophys. Res., 120(3), 480–501.
Keywords: driftwood, identification, morphological characteristics, origin, Nunavik, Hudson Bay, 0439 Ecosystems: structure and dynamics, 0460 Marine systems, 0476 Plant ecology, 0499 New fields (not classifiable under other headings),
Programme: 1080
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Beans C., Hecq J.H., Koubbi P., Vallet C., Wright S., Goffart A. (2008). A study of the diatom-dominated microplankton summer assemblages in coastal waters from Terre Adélie to the. Mertz Glacier, East Antarctica (139°E–145°E). Polar Biol., 3, 1101–1117.
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Nishitani, N.; Ogawa, T.; Sato, N.; Yamagishi, H.; Pinnock, M.; Villain, J.-P.; Sofko, G.; Troshichev, O. (2002). A study of the dusk convection cell's response to an IMF southward turning. J. Geophys. Res., 107.
Abstract: One example of the response of ionospheric convection and the polar cap boundary to a sudden change in the interplanetary magnetic field (IMF) orientation has been studied by using ground magnetometers, the Super Dual Auroral Radar Network (SuperDARN), and Defense Meteorological Satellite Program (DMSP) particle detectors when the IMF suddenly changed from northward (+6 nT) to strongly southward (?19 nT) at 1716 UT on 5 September 1995. The Bz component was fairly constant for ?2 hours before and ?25 min after the sudden IMF change. The convection flow changed almost simultaneously over a global extent. This initial change of the convection pattern can be characterized by a sudden formation of a large flow vortex in the afternoon sector. This agrees with the earlier findings by Ruohoniemi and Greenwald [1998] and Ridley et al. [1998]. On the other hand, the response of the polar cap boundary (or its proxy) is more complicated. The Saskatoon radar, located in the late morning sector, observed an equatorward shift of the cusp scatter region simultaneously with the initial response of the convection flows. The DMSP particle data also showed a simultaneous equatorward expansion of the auroral oval in the 2100 magnetic local time (MLT) sector. The radar and particle data indicate the immediate equatorward expansion of the precipitation regions in the noon and premidnight sectors. About 10–20 min after the initial change, there were changes observed in the dusk region, namely, an equatorward expansion of the current reversal boundary observed by the Greenland magnetometer chain in the dusk sector between 1740 and 1750 UT and an equatorward expansion of the convection reversal boundary detected by the Stokkseyri, Halley, and Syowa radars. The delayed responses were observed 18-8 min before a substorm onset was recorded at midlatitude stations at 1756 UT. These observations indicate that there were two kinds of ionospheric responses to the southward turning of the IMF; the first response is the formation of the convection vortex and the equatorward shift of the polar cap boundary at noon and at ?2100 MLT, and the second response is the equatorward expansion of the convection reversal boundary in the dusk sector. We make the case that the first response is associated with the propagation of magnetosonic waves and that the second response is consistent with the Cowley and Lockwood [1992] picture of the redistribution of the newly created open flux in the polar cap region.
Keywords: 2463 Ionosphere: Plasma convection; 2431 Ionosphere: Ionosphere/magnetosphere interactions; 2437 Ionosphere: Ionospheric dynamics; 2784 Magnetospheric Physics: Solar wind/magnetosphere interactions
Programme: 312;911
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