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. (2001). Ice sheet and radar altimetry. Surveys in geophysics, 22.
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Mandea M. & Purucker M. (2005). Observing, modeling, and interpreting magnetic fields of the solid earth. Surveys in geophysics, 26, 415–459.
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Chisham, G.; Lester, M.; Milan, S. E.; Freeman, M. P.; Bristow, W. A.; Grocott, A.; McWilliams, K. A.; Ruohoniemi, J. M.; Yeoman, T. K.; Dyson, P. L.; Greenwald, R. A.; Kikuchi, T.; Pinnock, M.; Rash, J. P. S.; Sato, N.; Sofko, G. J.; Villain, J.-P.; Walk. (2007). A decade of the Super Dual Auroral Radar Network (SuperDARN): scientific achievements, new techniques and future directions. Surveys in geophysics, 28, 33–109.
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Mioara Mandea, Aude Chambodut. (2020). Geomagnetic Field Processes and Their Implications for Space Weather (Vol. 41).
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S. Jevrejeva, A. Matthews, A. Slangen. (2017). The Twentieth-Century Sea Level Budget: Recent Progress and Challenges (Vol. 38).
Keywords: Data archeology Observing system Sea level budget Sea level rise
Programme: 688
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. (2019). Coastal Sea Level and Related Fields from Existing Observing Systems (Vol. 40).
Abstract: We review the status of current sea-level observing systems with a focus on the coastal zone. Tide gauges are the major source of coastal sea-level observations monitoring most of the world coastlines, although with limited extent in Africa and part of South America. The longest tide gauge records, however, are unevenly distributed and mostly concentrated along the European and North American coasts. Tide gauges measure relative sea level but the monitoring of vertical land motion through high-precision GNSS, despite being essential to disentangle land and ocean contributions in tide gauge records, is only available in a limited number of stations. (25% of tide gauges have a GNSS station at less than 10 km.) Other data sources are new in situ observing systems fostered by recent progress in GNSS data processing (e.g., GPS reflectometry, GNSS-towed platforms) and coastal altimetry currently measuring sea level as close as 5 km from the coastline. Understanding observed coastal sea level also requires information on various contributing processes, and we provide an overview of some other relevant observing systems, including those on (offshore and coastal) wind waves and water density and mass changes.
Programme: 688
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. (2002). Heavy-ion induced defects in phlogopite imaged by scanning force microscopy. Surface & coatings technology, 158-159, 439–443.
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Foucault, E., P.-l. Blelly, A. Marchaudon. (2017). High frequency waves propagation in Earth ionosphere.
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Marchaudon, A., P.-l. Blelly, F. Pitout, M. Indurain, A. Goutenoir, V. Génot, N. André, L. Beigbeder, M. Bouchemit, S. Caussarieu, N. Dufourg, J. Durand, M. Gangloff, D. Popescu, J.-p. Toniutti. (2017). Development of new ionospheric on-line tools in the frame of CDPP.
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Marchaudon, A., M. Grandin, P.-l. Blelly, A. Aikio, A. Kozlovsky, I. Virtanen, H. Vanhamäki. (2017). Modelling of a HSS event impact on the high latitude ionosphere.
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