Due to its inherent characteristics, the Instrument allows for a whole new spectrum of data collection and analysis, as well as for the optimization of the research being carried out in complex environments.

 

Faculty of the Rosenstiel School of Marine and Atmospheric Science at the University of Miami [http://www.rsmas.miami.edu/], as stated in their commitment letter, will utilize the Instrument for research and education efforts in Coastal Studies.

 

Coastal research by the team of Nelson Melo [http://CAKE.fiu.edu/Melo] at FIU and their extramural colleagues will utilize the instrument research in the fields of oceanography and marine remote sensing. In particular, it will provide new ways to study oceanic surface and sub-surface phenomena.

 

One of the challenges in airborne remote sensing of the water and coastal environment is the interference of the atmosphere [I. Levin; Chuanmin Hu; W. Zhang]. Because water targets are typically dark, an accurate atmospheric correction is required. Such a correction, however, is often difficult because of the unknown thickness of altitude of aerosol. These unknowns are often assumed "known", based on historical values but the errors involved on those "corrections" often mask the data needed aerosols [Gordon, H.; Mao, Z. (2013), Mao, Z. (2014)]. The Instrument's low flight heights (less than 500 ft) and no-vibration, slow-flight speeds will minimize such interference and reduce blurring of the high-spatial resolution (1-10 cm) pixels needed to obtain mutli-temporal aerial photography (color, panchromatic and multispectral) and integrate this data with up to 12 ancillary sensors.

 

Sandy beaches provide a natural barrier between the ocean and inland communities, ecosystems, and resources. However, these dynamic environments move and change in response to winds, waves, and currents. During a hurricane, these changes can be large and sometimes catastrophic. High waves and storm surge act together to erode beaches and inundate low-lying lands, putting inland communities at risk [Doran, K.S.]. The Instrument will enable the identification of coastline areas likely to experience extreme and potentially hazardous erosion during a hurricane, as well as low-cost quick response to post-disaster coastal change.

 

The Dominican Republic Universidad Tecnológica de Santiago's Center for Energy Studies will utilize the Instrument for analytics of hyper-spectral near-coastal aerial imagery to detect areas of cold water at sea bed. This would allow piping of that water into the chilling system on shore, resulting in tremendous saving on electricity for air-conditioning for large installations.

 

 

References Cited

 

[LL07] I. Levin and E. Levina, "Effect of atmospheric interference and sensor noise in retrieval of optically active materials in the ocean by hyperspectral remote sensing," Appl. Opt. 46, 6896-6906 (2007).

[HC02] C. Hu and K. Carder, Atmospheric correction for airborne sensors: Comment on a scheme used for CASI, Remote Sensing of Environment, Volume 79, Issue 1, January 2002, Pages 134-137, ISSN 0034-4257

[RZ07] J. Ruan and W. Zhang. An efficient spectral algorithm for network community discovery and its applications to biological and social networks. In ICDM, 2007.

[GW94] H.R. Gordon and M. Wang. "Retrieval of water-leaving radiance and aerosol optical thickness over the oceans with SeaWiFS: a preliminary algorithm." Applied optics 33, no. 3 (1994): 443-452.

[MAO+13] Z. Mao, et al. "A new approach to estimate the aerosol scattering ratios for the atmospheric correction of satellite remote sensing data in coastal regions." Remote Sensing of Environment 132 (2013): 186-194.

[MAO+14] Z. Mao, et al. "A potentially universal algorithm for estimating aerosol scattering reflectance from satellite remote sensing data." Remote Sensing of Environment 142 (2014): 131-140.

[SFL+12] K.S. Doran, H.F. Stockdon, K.L. Sopkin, D.M. Thompson, and N.G. Plant, 2012, National assessment of hurricane-induced coastal erosion hazards: Mid-Atlantic Coast: U.S. Geological Survey Open-File Report 2013-1131, 28 p.