French Polar Institute Literature Database -- Query Results

. (2017). (Vol. 349). Programme: 1003 http://publi.ipev.fr/polar_references/show.php?record=6750
. (2009). Nitrogen and carbon isotope values of individual amino acids: a tool to study foraging ecology of penguins in the Southern Ocean. Mar. Ecol. Prog. Ser., 391, 293–306. Programme: 109 http://publi.ipev.fr/polar_references/show.php?record=1931
O. I. Berngardt, J. M. Ruohoniemi, J.-P. St?Maurice, A. Marchaudon, M. J. Kosch, A. S. Yukimatu, N. Nishitani, S. G. Shepherd, M. F. Marcucci, H. Hu, T. Nagatsuma, M. Lester. (2019). Global Diagnostics of Ionospheric Absorption During X-Ray Solar Flares Based on 8- to 20-MHz Noise Measured by Over-the-Horizon Radars (Vol. 17). Bachelor's thesis, , . Keywords: \special t4ht@.D layer; \special t4ht@.E layer; decameter radars; ionosphere; radionoise absorption; X-ray solar flares Programme: 312 http://publi.ipev.fr/polar_references/show.php?record=7476
. (2010). Population genetics of 17 Y-chromosomal STR loci in Yakutia . Forensic Sci Int Genet, 4(5), e129–e130. Keywords: Y-Chromosomal STR, Haplotype, AmpFlSTR Yfiler, Yakut population, Programme: 1038 http://publi.ipev.fr/polar_references/show.php?record=2689
Pol K, Masson-Delmotte V, Johnsen S, Bigler M, Cattani O, Durand G, Falourd S, Jouzel J, Minster B, Parrenin F, Ritz C, Steen-Larsen HC, Stenni B, . (2010). New MIS 19 EPICA Dome C high resolution deuterium data: Hints for a problematic preservation of climate variability at sub-millennial scale in the “oldest ice” . Earth Planet. Sci. Lett., 298(1-2), 95–103. Keywords: water stable isotopes, ice cores, Antarctica, isotopic diffusion, Programme: 902 http://publi.ipev.fr/polar_references/show.php?record=2009
Pol K, Masson-Delmotte V, Johnsen S, Bigler M, Cattani O, Durand G, Falourd S, Jouzel J, Minster B, Parrenin F, Ritz C, Steen-Larsen HC, Stenni B, . (2010). New MIS 19 EPICA Dome C high resolution deuterium data: Hints for a problematic preservation of climate variability at sub-millennial scale in the “oldest ice” . Earth Planet. Sci. Lett., 298(1-2), 95–103. Keywords: water stable isotopes, ice cores, Antarctica, isotopic diffusion, Programme: 458 http://publi.ipev.fr/polar_references/show.php?record=2717
Descamps S., Gauthier-Clerc M., Le Bohec C., Gendner J.P. & Le Maho Y. (2005). Impact of predation on King penguin Aptenodytes patagonicus in Crozet archipelago. Polar Biol., 28(4), 303–310. Keywords: Vertebrata ; Climatic zone ; Aptenodytes patagonicus ; Aves ; Polar region ; Predation Programme: 137 http://publi.ipev.fr/polar_references/show.php?record=2902
De Lauretis M., Patrizia Francia, Andrea Piancatelli, Massimo Vellante, Umberto Villante. (2009). Low and mid-frequency pulsations in the polar cap: polarization pattern and MLT dependence of the spectral power during the descending phase of the solar cycle. Annals of geophysics, 52(1), 27–34. Keywords: ULF waves; Antarctica; Geomagnet; ic pulsations; Polarization pattern; upstream waves Programme: 1130 http://publi.ipev.fr/polar_references/show.php?record=5371
Geoffroy, L.; Aubourg, C.; Callot, J.-P.; Barrat, J.-A. (2007). Mechanisms of crustal growth in large igneous provinces: The north Atlantic province as a case study. Geological Society of America Special Papers, 430, 747–774. Abstract: The mechanisms of magma crust accretion at large igneous provinces (LIPs) are questioned using arguments based on the north Atlantic case. Published and new data on the calculated flow vectors within dike swarms feeding the early traps and subsequent seaward-dipping reflector lavas suggest that most of the mafic magmas forming the north Atlantic LIP transited through a small number of igneous centers. The magma was injected centrifugally in dike swarms at some distance away from individual igneous centers along the trend of the maximum horizontal stress acting in the crust, feeding lava piles via dikes intersecting the ground surface. This mechanism is similar to that observed in present-day Iceland and, more generally, in mafic volcano-tectonic systems. The absence of generalized vertical magma transit in a LIP has major geodynamic consequences. We cannot link the surface extent of LIP magmas to the dimensions of the mantle melting zone as proposed in former plume head models. The distribution of LIP magmas at the surface is primarily controlled by the regional stress field acting within the upper crust, but is also affected by magma viscosity. The igneous centers feeding LIPs most likely represent the crustal expression of small-scale convective cells of the buoyant mantle naturally located beneath the mechanical lithosphere. Keywords: traps; volcanic margin; dike swarm; small-scale convection; AMS Programme: 290 http://publi.ipev.fr/polar_references/show.php?record=5504
Koukouli M E, Lerot C, Granville J, Goutail F, Lambert J-C, Pommereau J-P, Balis D, Zyrichidou I, Van Roozendael M, Coldewey-Egbers M, Loyola D, Labow G, Frith S, Spurr R, Zehner C, . (2015). Evaluating a new homogeneous total ozone climate data record from GOME/ERS-2, SCIAMACHY/Envisat, and GOME-2/MetOp-A. Journal of Geophysical Research: Atmospheres, 120(23), 12,296–12,312. Abstract: The European Space Agency's Ozone Climate Change Initiative (O3-CCI) project aims at producing and validating a number of high-quality ozone data products generated from different satellite sensors. For total ozone, the O3-CCI approach consists of minimizing sources of bias and systematic uncertainties by applying a common retrieval algorithm to all level 1 data sets, in order to enhance the consistency between the level 2 data sets from individual sensors. Here we present the evaluation of the total ozone products from the European sensors Global Ozone Monitoring Experiment (GOME)/ERS-2, SCIAMACHY/Envisat, and GOME-2/MetOp-A produced with the GOME-type Direct FITting (GODFIT) algorithm v3. Measurements from the three sensors span more than 16 years, from 1996 to 2012. In this work, we present the latest O3-CCI total ozone validation results using as reference ground-based measurements from Brewer and Dobson spectrophotometers archived at the World Ozone and UV Data Centre of the World Meteorological Organization as well as from UV-visible differential optical absorption spectroscopy (DOAS)/Système D′Analyse par Observations Zénithales (SAOZ) instruments from the Network for the Detection of Atmospheric Composition Change. In particular, we investigate possible dependencies in these new GODFIT v3 total ozone data sets with respect to latitude, season, solar zenith angle, and different cloud parameters, using the most adequate type of ground-based instrument. We show that these three O3-CCI total ozone data products behave very similarly and are less sensitive to instrumental degradation, mainly as a result of the new reflectance soft-calibration scheme. The mean bias to the ground-based observations is found to be within the 1 ± 1% level for all three sensors while the near-zero decadal stability of the total ozone columns (TOCs) provided by the three European instruments falls well within the 1–3% requirement of the European Space Agency's Ozone Climate Change Initiative project. Keywords: total ozone, SCIAMACHY, Brewer, Dobson, GOME-2, validation, 0340 Middle atmosphere: composition and chemistry, 0394 Instruments and techniques, 0480 Remote sensing, Programme: 209 http://publi.ipev.fr/polar_references/show.php?record=6317

. (2017). (Vol. 349).

. (2009). Nitrogen and carbon isotope values of individual amino acids: a tool to study foraging ecology of penguins in the Southern Ocean. Mar. Ecol. Prog. Ser., 391, 293–306.

O. I. Berngardt, J. M. Ruohoniemi, J.-P. St?Maurice, A. Marchaudon, M. J. Kosch, A. S. Yukimatu, N. Nishitani, S. G. Shepherd, M. F. Marcucci, H. Hu, T. Nagatsuma, M. Lester. (2019). Global Diagnostics of Ionospheric Absorption During X-Ray Solar Flares Based on 8- to 20-MHz Noise Measured by Over-the-Horizon Radars (Vol. 17). Bachelor's thesis, , .

. (2010). Population genetics of 17 Y-chromosomal STR loci in Yakutia . Forensic Sci Int Genet, 4(5), e129–e130.

Pol K, Masson-Delmotte V, Johnsen S, Bigler M, Cattani O, Durand G, Falourd S, Jouzel J, Minster B, Parrenin F, Ritz C, Steen-Larsen HC, Stenni B, . (2010). New MIS 19 EPICA Dome C high resolution deuterium data: Hints for a problematic preservation of climate variability at sub-millennial scale in the “oldest ice” . Earth Planet. Sci. Lett., 298(1-2), 95–103.

Descamps S., Gauthier-Clerc M., Le Bohec C., Gendner J.P. & Le Maho Y. (2005). Impact of predation on King penguin Aptenodytes patagonicus in Crozet archipelago. Polar Biol., 28(4), 303–310.

De Lauretis M., Patrizia Francia, Andrea Piancatelli, Massimo Vellante, Umberto Villante. (2009). Low and mid-frequency pulsations in the polar cap: polarization pattern and MLT dependence of the spectral power during the descending phase of the solar cycle. Annals of geophysics, 52(1), 27–34.

Geoffroy, L.; Aubourg, C.; Callot, J.-P.; Barrat, J.-A. (2007). Mechanisms of crustal growth in large igneous provinces: The north Atlantic province as a case study. Geological Society of America Special Papers, 430, 747–774.

Koukouli M E, Lerot C, Granville J, Goutail F, Lambert J-C, Pommereau J-P, Balis D, Zyrichidou I, Van Roozendael M, Coldewey-Egbers M, Loyola D, Labow G, Frith S, Spurr R, Zehner C, . (2015). Evaluating a new homogeneous total ozone climate data record from GOME/ERS-2, SCIAMACHY/Envisat, and GOME-2/MetOp-A. Journal of Geophysical Research: Atmospheres, 120(23), 12,296–12,312.

Abstract: The European Space Agency's Ozone Climate Change Initiative (O3-CCI) project aims at producing and validating a number of high-quality ozone data products generated from different satellite sensors. For total ozone, the O3-CCI approach consists of minimizing sources of bias and systematic uncertainties by applying a common retrieval algorithm to all level 1 data sets, in order to enhance the consistency between the level 2 data sets from individual sensors. Here we present the evaluation of the total ozone products from the European sensors Global Ozone Monitoring Experiment (GOME)/ERS-2, SCIAMACHY/Envisat, and GOME-2/MetOp-A produced with the GOME-type Direct FITting (GODFIT) algorithm v3. Measurements from the three sensors span more than 16 years, from 1996 to 2012. In this work, we present the latest O3-CCI total ozone validation results using as reference ground-based measurements from Brewer and Dobson spectrophotometers archived at the World Ozone and UV Data Centre of the World Meteorological Organization as well as from UV-visible differential optical absorption spectroscopy (DOAS)/Système D′Analyse par Observations Zénithales (SAOZ) instruments from the Network for the Detection of Atmospheric Composition Change. In particular, we investigate possible dependencies in these new GODFIT v3 total ozone data sets with respect to latitude, season, solar zenith angle, and different cloud parameters, using the most adequate type of ground-based instrument. We show that these three O3-CCI total ozone data products behave very similarly and are less sensitive to instrumental degradation, mainly as a result of the new reflectance soft-calibration scheme. The mean bias to the ground-based observations is found to be within the 1 ± 1% level for all three sensors while the near-zero decadal stability of the total ozone columns (TOCs) provided by the three European instruments falls well within the 1–3% requirement of the European Space Agency's Ozone Climate Change Initiative project.

Keywords: total ozone, SCIAMACHY, Brewer, Dobson, GOME-2, validation, 0340 Middle atmosphere: composition and chemistry, 0394 Instruments and techniques, 0480 Remote sensing,

Programme: 209

http://publi.ipev.fr/polar_references/show.php?record=6317