J.-Ch. Hamilton for the QUBIC Collaboration. (2013). QUBIC: The QU Bolometric Interferometer for Cosmology.
Abstract: Invited talk at CMB2013, held at Okinawa, Japan, 1-14 June 2013
Programme: 915
|
Marie-Anne Bigot-Sazy, for the QUBIC Collaboration. (2013). QUBIC: The QU Bolometric Interferometer for Cosmology.
Abstract: Invited talk at Cosmology in the Planck Era, held at Quy Nhon, Viet Nam, July 28th-Aug 3 2013
Programme: 915
|
Andrea Tartari for the QUBIC Collaboration. (2013). QUBIC: The QU Bolometric Interferometer for Cosmology.
Abstract: Contributed talk at AP-RASC'13 held in Taiwan, september 3-7 2013
Programme: 915
|
Adnan Ghribi for the QUBIC Collaboration. (2013). QUBIC: The QU bolometric Interferometer for Cosmology.
Abstract: Contributed talk at LTD15 held in Pasadena, California, USA, June 24th-28th 2013
Programme: 915
|
J.-Ch. Hamilton for the QUBIC Collaboration. (2013). QUBIC: The QU Bolometric Interferometer for Cosmology.
Abstract: Invited talk at SCAR-AAA workshop (Scientific Committee on Antarctic Research – Astronomy and Astrophysics from Antarctica), held in Siena, Italy, 24-26 july 2013
Programme: 915
|
T. Dinh, A. Podglajen, A. Hertzog, B. Legras, R. Plougonven. (2016). Effect of gravity wave temperature fluctuations on homogeneous ice nucleation in the tropical tropopause layer (Vol. 16).
Abstract: The impact of high-frequency fluctuations of temperature on homogeneous nucleation of ice crystals in the vicinity of the tropical tropopause is investigated using a bin microphysics scheme for air parcels. The imposed temperature fluctuations come from measurements during isopycnic balloon flights near the tropical tropopause. The balloons collected data at high frequency, guaranteeing that gravity wave signals are well resolved. With the observed temperature time series, the numerical simulations with homogeneous freezing show a full range of ice number concentration (INC) as previously observed in the tropical upper troposphere. In particular, a low INC may be obtained if the gravity wave perturbations produce a non-persistent cooling rate (even with large magnitude) such that the absolute change in temperature remains small during nucleation. This result is explained analytically by a dependence of the INC on the absolute drop in temperature (and not on the cooling rate). This work suggests that homogeneous ice nucleation is not necessarily inconsistent with observations of low INCs.
Programme: 914
|
Nathalie Boullot, Florence Rabier, Rolf Langland, Ron Gelaro, Carla Cardinali, Vincent Guidard, Peter Bauer, Alexis Doerenbecher. (2016). Observation impact over the southern polar area during the Concordiasi field campaign (Vol. 142).
Abstract: The impact of observations on analysis uncertainty and forecast performance was investigated for austral spring 2010 over the southern polar area for four different systems (NRL, GMAO, ECMWF and Météo-France) at the time of the Concordiasi field experiment. The largest multi-model variance in 500 hPa height analyses is found in the southern sub-Antarctic oceanic region, where there are rapidly evolving weather systems, rapid forecast-error growth, and fewer upper-air wind observation data to constrain the analyses. The total impact of all observations on the model forecast was computed using the 24 h forecast sensitivity-to-observations diagnostic. Observation types that contribute most to the reduction of the forecast error are shown to be AMSU, IASI, AIRS, GPS-RO, radiosonde, surface and atmospheric motion vector observations. For sounding data, radiosondes and dropsondes, one can note a large impact on the analysis and forecasts of temperature at low levels and a large impact of wind at high levels. Observing system experiments using the Concordiasi dropsondes show a large impact of the observations over the Antarctic plateau extending to lower latitudes with the forecast range, with the largest impact around 50–70°S. These experiments indicate there is a potential benefit from using radiance data better over land and sea-ice and from innovative atmospheric motion vectors obtained from a combination of various satellites to fill the current data gaps and improve numerical weather prediction analyses in this region.
Keywords: dropsondes forecast score forecast sensitivity to observations observing-system experiment
Programme: 914
|
André R. & Dudok de Wit T. (2003). Identification of the ionospheric footprint of magnetospheric boundaries using SuperDARN coherent HF radars. Planetary and space science, 51, 813–820.
|
LointierG, Dudok de WitT, HanuiseC, VallièresX, VillainJ-P, . (2008). A statistical approach for identifying the ionospheric footprint of magnetospheric boundaries from SuperDARN observations
. 0992-7689, 26(2), 305–314.
Abstract: Identifying and tracking the projection of magnetospheric regions on the high-latitude ionosphere is of primary importance for studying the Solar Wind-Magnetosphere-Ionosphere system and for space weather applications. By its unique spatial coverage and temporal resolution, the Super Dual Auroral Radar Network (SuperDARN) provides key parameters, such as the Doppler spectral width, which allows the monitoring of the ionospheric footprint of some magnetospheric boundaries in near real-time. In this study, we present the first results of a statistical approach for monitoring these magnetospheric boundaries. The singular value decomposition is used as a data reduction tool to describe the backscattered echoes with a small set of parameters. One of these is strongly correlated with the Doppler spectral width, and can thus be used as a proxy for it. Based on this, we propose a Bayesian classifier for identifying the spectral width boundary, which is classically associated with the Polar Cap boundary. The results are in good agreement with previous studies. Two advantages of the method are: the possibility to apply it in near real-time, and its capacity to select the appropriate threshold level for the boundary detection.
Programme: 911
|
Marchaudon A, Cerisier J-C, Dunlop M W, Pitout F, Bosqued J-M, Fazakerley A N, . (2009). Shape, size, velocity and field-aligned currents of dayside plasma injections: a multi-altitude study
. Ann. Geophys., 27(3), 1251–1266.
|