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Charrassin J.-B. et al. |
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Title ![sorted by Title field, ascending order (up)](img/sort_asc.gif) |
Animal-borne sensors reveal new ocean processes in polar regions |
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Conference - International - Article with Reading Comitee |
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2009 |
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White community papers, Ocean'Obs09, Venice, September 21-25, 2009 |
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452 |
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yes |
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6032 |
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Rob Harcourt, Ana M. M. Sequeira, Xuelei Zhang, Fabien Roquet, Kosei Komatsu, Michelle Heupel, Clive McMahon, Fred Whoriskey, Mark Meekan, Gemma Carroll, Stephanie Brodie, Colin Simpfendorfer, Mark Hindell, Ian Jonsen, Daniel P. Costa, Barbara Block, Mônica Muelbert, Bill Woodward, Mike Weise, Kim Aarestrup, Martin Biuw, Lars Boehme, Steven J. Bograd, Dorian Cazau, Jean-Benoit Charrassin, Steven J. Cooke, Paul Cowley, P. J. Nico de Bruyn, Tiphaine Jeanniard du Dot, Carlos Duarte, VÃctor M. EguÃluz, Luciana C. Ferreira, Juan Fernández-Gracia, Kimberly Goetz, Yusuke Goto, Christophe Guinet, Mike Hammill, Graeme C. Hays, Elliott L. Hazen, Luis A. Hückstädt, Charlie Huveneers, Sara Iverson, Saifullah Arifin Jaaman, Kongkiat Kittiwattanawong, Kit M. Kovacs, Christian Lydersen, Tim Moltmann, Masaru Naruoka, Lachlan Phillips, Baptiste Picard, Nuno Queiroz, Gilles Reverdin, Katsufumi Sato, David W. Sims, Eva B. Thorstad, Michele Thums, Anne M. Treasure, Andrew W. Trites, Guy D. Williams, Yoshinari Yonehara, Mike A. Fedak |
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Title ![sorted by Title field, ascending order (up)](img/sort_asc.gif) |
Animal-Borne Telemetry: An Integral Component of the Ocean Observing Toolkit |
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Journal |
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Year |
2019 |
Publication |
Frontiers in marine science |
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6 |
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Animal Movement Animal movement analysis Animal telemetry EOV habitat use Ocean observing |
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Abstract |
Animal telemetry is a powerful tool for observing marine animals and the physical environments that they inhabit, from coastal and continental shelf ecosystems to polar seas and open oceans. Satellite-linked biologgers and networks of acoustic receivers allow animals to be reliably monitored over scales of tens of meters to thousands of kilometres, giving insight into their habitat use, home range size, the phenology of migratory patterns and the biotic and abiotic factors that drive their distributions. Furthermore, physical environmental variables can be collected using animals as autonomous sampling platforms, increasing spatial and temporal coverage of global oceanographic observation systems. The use of animal telemetry therefore has the capacity to provide measures from a suite of essential ocean variables (EOVs) for improved monitoring of Earth’s oceans. Here we outline the design features of animal telemetry systems, describe current applications and their benefits and challenges, and discuss future directions. We describe new analytical techniques that improve our ability to not only quantify animal movements but to also provide a powerful framework for comparative studies across taxa. We discuss the application of animal telemetry and its capacity to collect biotic and abiotic data, how the data collected can be incorporated into ocean observing systems, and the role these data can play in improved ocean management. |
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109,1182,1201 |
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Bachelor's thesis |
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2296-7745 |
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2296-7745 |
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yes |
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7459 |
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Castelnau O., Shoji H., Mangeney A., Milsch H., Duval P., Miyamoto A., Kawada K. & Watanabe O. |
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Title ![sorted by Title field, ascending order (up)](img/sort_asc.gif) |
Anisotropic behavior of Grip ices and flow in central Greenland. |
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Journal Article |
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Year |
1998 |
Publication |
Earth and planetary science letters |
Abbreviated Journal |
Earth Planet. Sci. Lett. |
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154 |
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Pages |
307-322 |
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322 |
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0012-821X |
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yes |
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657 |
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Lev Vinnik, Sergey Oreshin, Larissa Makeyeva, Dmitriy Peregoudov, Elena Kozlovskaya, Elena Kozlovskaya, Helle Pedersen, Jaroslava Plomerova, Ulrich Achauer, Eduard Kissling, Irina Sanina, Teppo Jämsen, Hanna Silvennoinen, Catherine Pequegnat, Riitta Hurskainen, Robert Guiguet, Helmut Hausmann, Petr Jedlicka, Igor Aleshin, Ekaterina Bourova, Reynir Bodvarsson, Evald Brückl, Tuna Eken, Pekka Heikkinen, Gregory Houseman, Helge Johnsen, Elena Kremenetskaya, Kari Komminaho, Helena Munzarova, Roland Roberts, Bohuslav Ruzek, Hossein Shomali, Johannes Schweitzer, Artem Shaumyan, Ludek Vecsey, Sergei Volosov |
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Title ![sorted by Title field, ascending order (up)](img/sort_asc.gif) |
Anisotropic lithosphere under the Fennoscandian shield from P receiver functions and SKS waveforms of the POLENET/LAPNET array |
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Journal |
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2014 |
Publication |
Tectonophysics |
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628 |
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45-54 |
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Keywords |
Asthenosphere Lithosphere Mantle flow Receiver functions Seismic anisotropy Shear-wave splitting |
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Abstract |
Seismic azimuthal anisotropy is the key evidence of the past and present strains in the upper mantle. The standard analysis of shear-wave splitting with the SKS techniques is useful in mapping lateral variations but it is insensitive to depth of anisotropy and to variations of anisotropy with depth. To retrieve the depth localized anisotropy under the Fennoscandian shield, we inverted P-wave receiver functions of the POLENET/LAPNET array in northern Finland jointly with SKS recordings. Shear-wave anisotropy of ~2.5% with the fast direction of 40°–60° in a depth range from the Moho to ~110km is a robust result of the inversion. The obtained direction is nearly normal to the azimuth of the maximum horizontal compressional stress in the lithosphere, but a recent origin of this anisotropy is in doubt. This anisotropy may be frozen since the Precambrian, but it shows no clear relation with the trends of the Precambrian tectonics. The upper anisotropic layer accounts for ~40% of shear-wave splitting in SKS, and to explain the rest another anisotropic layer is required. The top of the second layer with a practically similar fast direction is found at a depth of 200–240km. This direction is close to the current APM direction of the lithosphere with implication that the inferred anisotropy may be related with the current plate motion, and the anisotropic layer belongs to the asthenosphere. The bottom of this layer is uncertain, but it is at least 320km deep. In a depth range from 160km to 200–240km the fast anisotropy direction is 110–150°. Origin of this direction is unclear. |
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1021 |
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0040-1951 |
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yes |
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8169 |
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Author |
Gresillaud A. & Cara M. |
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Anisotropy and P-wave tomography : a new approach for inverting teleseismic data from dense array of stations. |
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Journal Article |
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1996 |
Publication |
Geophysical journal international |
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126 |
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77-91 |
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133 |
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0956-540X |
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yes |
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1103 |
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Author |
Souriau A. & Romanowicz B. |
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Title ![sorted by Title field, ascending order (up)](img/sort_asc.gif) |
Anisotropy in inner core attenuation : a new type of data to constrain the nature of the solid core. |
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Journal Article |
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1996 |
Publication |
Geophysical research letters |
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23 |
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133 |
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0094-8276 |
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yes |
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1780 |
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Levêque J.J., Debayle E. & Maupin V. |
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Anisotropy in the Indian ocean upper mantle from Rayleigh- and Love waveform inversion. |
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Journal Article |
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1998 |
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Geophysical journal international |
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133 |
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529-540 |
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133 |
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0956-540X |
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177 |
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Vernon P., Caron F. & Davies L. |
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Annual activity of two endemic beetles (Carabidae) at the edge between fell-field and moorland on a sub-Antarctic island. |
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Journal Article |
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1999 |
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European journal of soil biology |
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Eur. J. Soil Biol. |
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35 |
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1 |
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39-43 |
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136 |
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1164-5563 |
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yes |
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887 |
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Kopczynska E., Fiala M. & Jeandel C. |
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Title ![sorted by Title field, ascending order (up)](img/sort_asc.gif) |
Annual and interannual variability in phytoplankton abundance and composition at a permanent station Kerfix off Kerguelen Islands, the Southern Ocean. |
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Journal Article |
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Year |
1998 |
Publication |
Polar biology |
Abbreviated Journal |
Polar Biol. |
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20 |
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342-351 |
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193 |
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0722-4060 |
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1592 |
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Descamps S., Gauthier-Clerc M., Gendner J.P. & Le Maho Y. |
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Title ![sorted by Title field, ascending order (up)](img/sort_asc.gif) |
Annual breeding cycle of unbanded king penguins Aptenodytes patagonicus on Possession Island (Crozet). |
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Journal Article |
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2002 |
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Avian science |
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2 |
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87-98 |
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137 |
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yes |
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1228 |
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