Titlebook: Meteorological Tsunamis: The U.S. East Coast and Other Coastal Regions; Ivica Vilibi?,Sebastian Monserrat,Alexander B. Rab Book 2015 Sprin

Living-Will

A. Frère,C. Daubord,A. Gailler,H. Hébertntary on, Ramanujan‘s results.In the spring of 1976, George Andrews of Pennsylvania State University visited the library at Trinity College, Cambridge, to examine the papers of the late G.N. Watson. Among these papers, Andrews discovered a sheaf of 138 pages in the handwriting of Srinivasa Ramanujan

遭遇

tenosynovitis

Accessible

有毛就脫毛

Charitha Pattiaratchi,E. M. S. Wijeratneiscoveries without proofs in notebooks. Although many of his results were already found in the literature, most were not. Almost a decade after Ramanujan‘s death in 1920, G.N. Watson and B.M. Wilson began to edit Ramanujan‘s notebooks, but they never completed the task. A photostat edition, with no

moribund

大罵

Atmospheric processes responsible for generation of the 2008 Boothbay meteotsunami,ober 2008. The data collected by tide gauges, ground and sounding stations and meteo–ocean buoys in the area were analyzed, together with satellite and radar images. The atmospheric processes were reproduced by the weather research and forecasting model, verified by in situ and remote sensing data.

Mercurial

Atmospheric mesoscale conditions during the Boothbay meteotsunami: a numerical sensitivity study usring the Boothbay Harbor meteotsunami on 28 October 2008. The simulations were performed by the Weather and Research Forecasting (WRF) model at 1-km horizontal grid spacing by varying initial conditions (ICs) and lateral boundary conditions (LBCs), nesting strategy, simulation lead time and microphy

Keratectomy

密切關(guān)系

High-frequency radar observations of the June 2013 US East Coast meteotsunami, tide gauges. This work extends the previous observations of tsunamis originating in Japan and Indonesia. The radars observed the meteotsunami 23?km offshore, 47?min before it arrived at the coast. Subsequent observations showed it moving onshore. The neighboring tide gauge height reading provides c