Higher waves along U.S. East Coast linked to hurricanes

Eos

Volumn 88, Issue 30, 2007, Pages 301-

  Komar, Paul D ^a   Allan, Jonathan C ^b  

^a OREGON STATE UNIVERSITY   (United States)

^b Oregon Department of Geology and Mineral Industries   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BUOY SYSTEM; HURRICANE; OCEAN WAVE; WAVE GENERATION; WAVE HEIGHT;

ATLANTIC COAST [NORTH AMERICA]; ATLANTIC COAST [UNITED STATES]; NORTH AMERICA; UNITED STATES;

EID: 34548588454     PISSN: 00963941     EISSN: None     Source Type: Journal    
DOI: 10.1029/2007EO300001     Document Type: Article

References (5)

1. Allan. J.C., and P.D. Komar (2000), Areocan wave heights increasing in the eastern North Pacific?. Eos Trans AGU. 81(47). 561. 566-567,
2. Allan. J. C.. and P. D Komar (2006), Climate controls on US West Coast erosion processes. J. Coastal Res. 22, 511-529.
3. Emanuel. K, A. (2005). Increasing destructiveness of tropical cyclones over the past 30 years Nature, 136, 686-688.
4. Landsea, C W. B. A. Harper, K. Hoarau. and J. A. Knaff (2006). Can we detect trends of extreme tropical cyclones?. Science, 313, 452-454.
5. Smith. J.J., R. Dolan. and H. Lins (2006). Hurricane history of the North Carolina Outer Banks (USA), 1586 to 2004, Shore Beach, 74(3). 19-23.