TY - JOUR
T1 - Requirements for a coastal hazards observing system
AU - Benveniste, Jérôme
AU - Cazenave, Anny
AU - Vignudelli, Stefano
AU - Fenoglio-Marc, Luciana
AU - Shah, Rashmi
AU - Almar, Rafael
AU - Andersen, Ole
AU - Birol, Florence
AU - Bonnefond, Pascal
AU - Bouffard, Jérôme
AU - Calafat, Francisco
AU - Cardellach, Estel
AU - Cipollini, Paolo
AU - Le Cozannet, Gonéri
AU - Dufau, Claire
AU - Fernandes, Maria Joana
AU - Frappart, Frédéric
AU - Garrison, James
AU - Gommenginger, Christine
AU - Han, Guoqi
AU - Høyer, Jacob L.
AU - Kourafalou, Villy
AU - Leuliette, Eric
AU - Li, Zhijin
AU - Loisel, Hubert
AU - Madsen, Kristine S.
AU - Marcos, Marta
AU - Melet, Angélique
AU - Meyssignac, Benoît
AU - Pascual, Ananda
AU - Passaro, Marcello
AU - Ribó, Serni
AU - Scharroo, Remko
AU - Song, Y. Tony
AU - Speich, Sabrina
AU - Wilkin, John
AU - Woodworth, Philip
AU - Wöppelmann, Guy
PY - 2019
Y1 - 2019
N2 - Coastal zones are highly dynamical systems affected by a variety of natural and anthropogenic forcing factors that include sea level rise, extreme events, local oceanic and atmospheric processes, ground subsidence, etc. However, so far, they remain poorly monitored on a global scale. To better understand changes affecting world coastal zones and to provide crucial information to decision-makers involved in adaptation to and mitigation of environmental risks, coastal observations of various types need to be collected and analyzed. In this white paper, we first discuss the main forcing agents acting on coastal regions (e.g., sea level, winds, waves and currents, river runoff, sediment supply and transport, vertical land motions, land use) and the induced coastal response (e.g., shoreline position, estuaries morphology, land topography at the land-sea interface and coastal bathymetry). We identify a number of space-based observational needs that have to be addressed in the near future to understand coastal zone evolution. Among these, improved monitoring of coastal sea level by satellite altimetry techniques is recognized as high priority. Classical altimeter data in the coastal zone are adversely affected by land contamination with degraded range and geophysical corrections. However, recent progress in coastal altimetry data processing and multi-sensor data synergy, offers new perspective to measure sea level change very close to the coast. This issue is discussed in much detail in this paper, including the development of a global coastal sea-level and sea state climate record with mission consistent coastal processing and products dedicated to coastal regimes. Finally, we present a new promising technology based on the use of Signals of Opportunity (SoOp), i.e., communication satellite transmissions that are reutilized as illumination sources in a bistatic radar configuration, for measuring coastal sea level. Since SoOp technology requires only receiver technology to be placed in orbit, small satellite platforms could be used, enabling a constellation to achieve high spatio-temporal resolutions of sea level in coastal zones.
AB - Coastal zones are highly dynamical systems affected by a variety of natural and anthropogenic forcing factors that include sea level rise, extreme events, local oceanic and atmospheric processes, ground subsidence, etc. However, so far, they remain poorly monitored on a global scale. To better understand changes affecting world coastal zones and to provide crucial information to decision-makers involved in adaptation to and mitigation of environmental risks, coastal observations of various types need to be collected and analyzed. In this white paper, we first discuss the main forcing agents acting on coastal regions (e.g., sea level, winds, waves and currents, river runoff, sediment supply and transport, vertical land motions, land use) and the induced coastal response (e.g., shoreline position, estuaries morphology, land topography at the land-sea interface and coastal bathymetry). We identify a number of space-based observational needs that have to be addressed in the near future to understand coastal zone evolution. Among these, improved monitoring of coastal sea level by satellite altimetry techniques is recognized as high priority. Classical altimeter data in the coastal zone are adversely affected by land contamination with degraded range and geophysical corrections. However, recent progress in coastal altimetry data processing and multi-sensor data synergy, offers new perspective to measure sea level change very close to the coast. This issue is discussed in much detail in this paper, including the development of a global coastal sea-level and sea state climate record with mission consistent coastal processing and products dedicated to coastal regimes. Finally, we present a new promising technology based on the use of Signals of Opportunity (SoOp), i.e., communication satellite transmissions that are reutilized as illumination sources in a bistatic radar configuration, for measuring coastal sea level. Since SoOp technology requires only receiver technology to be placed in orbit, small satellite platforms could be used, enabling a constellation to achieve high spatio-temporal resolutions of sea level in coastal zones.
KW - Coastal modeling
KW - Coastal zone
KW - Hazards
KW - Reflectometry Wideband Signals of Opportunity (GNSS-R/W-SoOp)
KW - Retracking
KW - SAR/Delay-Doppler Radar Altimetry
KW - Sea level
KW - Storm surge
U2 - 10.3389/fmars.2019.00348
DO - 10.3389/fmars.2019.00348
M3 - Review
AN - SCOPUS:85067080705
SN - 2296-7745
VL - 6
JO - Frontiers in Marine Science
JF - Frontiers in Marine Science
IS - JUL
M1 - 348
ER -