Geoscience Reference
In-Depth Information
Maki M., & Doviak, R. J. (2001). Volcanic ash size distribution determined by weather radar.
IEEE Int. Geosc. Rem. Sens. Symp., IGARSS '01
., 2001, vol.4, pp. (1810 - 1811), doi:
10.1109/IGARSS.2001.977079.
Maki M., Iwanami, K., Misumi, R., Doviak, R. J., Wakayama, T., Hata, K., & Watanabe, S.
(2001). Observation of volcanic ashes with a 3-cm polarimetric radar.
Proc. 30th
Radar Meteorol. Conf.
, 18-24 July, Munich, Germany, P5.13, p. (226-228).
Malassingne, C., Lemaitre, F., Briole, P., & Pascal, O. (2001). Potential of ground based
radar for the monitoring of deformation of volcanoes.
Geophys. Res. Lett
. 28, 851-
854.
Marzano, F.S., & Ferrauto, G. (2003). Relation between weather radar equation and first-
order backscattering theory.
Atmos. Chem. Phys
., 3, pp. (813-821).
Marzano, F. S., Barbieri, S., Vulpiani G., & Rose W.I. (2006a). Volcanic ash cloud retrieval by
ground-based microwave weather radar.
IEEE Trans. Geosc. Remote Sens.
, 44 (11),
pp. (3235-3246), doi:10.1109/TGRS.2006.879116.
Marzano, F.S., Vulpiani, G., & Rose W.I. (2006b). Microphysical characterization of
microwave radar reflectivity due to volcanic ash clouds.
IEEE Trans. Geosc. Remote
Sens.
, 44, pp. (313-327), doi:10.1109/TGRS.2005.861010.
Marzano, F.S., Barbieri, S., Picciotti, E., & Karlsdóttir, S. (2010a). Monitoring sub-glacial
volcanic eruption using C band radar imagery.
IEEE Trans. Geosc. Remote Sens.
, 48,
1, pp. (403-414).
Marzano, F. S., Marchiotto, S., Barbieri, S., Textor, C., & Schneider, D. (2010b). Model-based
Weather Radar Remote Sensing of Explosive Volcanic Ash Eruption,
IEEE Trans.
Geosc. Remote Sens.
, 48, pp. (3591-3607).
Marzano, F. S., Lamantea, M., Montopoli, M., Di Fabio, S., & Picciotti, E. (2011). The Eyjafjöll
explosive volcanic eruption from a microwave weather radar perspective.
Atmos.
Chem. Phys. Discuss
., 11, pp. (12367-12409), doi:10.5194/acpd-11-12367-2011.
Marzano, F. S., Picciotti, E., Vulpiani, G., & Montopoli, M. (2012). Synthetic signatures of
volcanic ash cloud particles from X-band dual-polarization radar.
IEEE Trans.
Geosc. Remote Sens.
, 50, 1, pp. (193-211).
Mastin, L. G., Guffanti, M., Servranckx, R., Webley, P., et al. (2009). A multidisciplinary
effort to assign realistic source parameters to models of volcanic ash cloud
transport and dispersion during eruptions.
J. Volcanol. Geotherm. Res
., 186, pp. (10-
21).
Mie, G. (1908). Beiträge zur Optik trüber Medien, speziell kolloidaler Metallösungen.
Ann.
Phys
., 330, 3, pp. (377-445).
Mora, M.M., Lesage, P., Donnadieu, F., Valade, S., Schmidt, A., Soto, G., Taylor, W., &
Alvarado, G. (2009). Joint Seismic, Acoustic and Doppler Radar observations at
Arenal Volcano, Costa Rica: preliminary results. In:
The VOLUME project
, Bean, C.
J., Braiden, A. K., Lokmer, I., Martini, F., & O'Brien, G. S. , pp. (330-340), VOLUME
Project Consortium, ISBN 978-1-905254-39-2, Dublin.
Musolf,M. (1994). Airborne radar detection of volcanic ash.
In
: First International
Symposium on Volcanic Ash and Aviation Safety, Casadevall, T.J. (Ed.),
U.S. Geol.
Surv. Bull., 2047
, pp. (387-390), Seattle, Washington, U.S.A.