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ƘĢćȩŦɦ,ǵ60Ĥ,2016ĩ2Ŷ `  t@Ïf¡cV ÕVÆ£ÄC{\±WG¤q SEASONAL VARIABILITY OF LAND-DERIVED PASSIVE TRACER DISPERSAL IN THE SETO INLAND SEA AND THE ENSHU-NADA COAST ©ė ɥ 1 oɗƜ Ƥÿ 2 oĔǟ þî 2 Yusuke UCHIYAMA, Yota SUZUE and Taichi KOSAKO 1 Ƒâ ÊĢ ǣŌþćþćɣšŕ ĢćǞǮǨĥƖĢćĒŞɷ657-8501 ǣŌĥƾħǎÔǏ1-1ɸ 2 ćNjâ ǣŌþćþćɣ ĢćǞǮǨĥƖĢćĒŞɷ657-8501 ǣŌĥƾħǎÔǏ1-1ɸ Coastal marginal seas and estuaries are generally dumpsites for wastewater from sewage and power plants. For an urgent assessment of dilution and dispersal of toxic materials due to accidental leakage, we develop an offline passive tracer model by exploiting oceanic reanalysis products and analyze differences in spatiotemporal variability of the leaked tracers in an estuary and a continental shelf margin on the Pacific side of Japan. In the estuary, the northeastward through flow affects the dispersal, while the month-long transport is dominated rather by inter-seasonal variability of wind-driven Ekman flow and counter-clockwise local circulations associated with the cold-dome density structure. On the marginal coast, the Kuroshio and resultant secondary recirculation readily entrain the tracer, leading to immediate transport mostly in the alongshore direction. The seasonal difference in the tracer dispersal is apparent such as sporadic offshore tracer eruption episodes, depending on the locations of the Kuroshio path. Key Words : ROMS, coastal dispersal, offline Eulerian passive tracer model, Kuroshio, Seto Inland Sea 1. ŋé%,ËĄ¸ǔɩŎ8uƘLjö+ýƠě) Ȥȉ=$);ɹƠěƫò,=:+ŪȤ:+ŖƘ+ ĮƆö&(!$< 1) ɺvƱ+}Ň)9!$.&/ŷ čǂȳ+ƹƧȵ=- 2) ɹƠěljø8NjŇǽ)ɓþ( ĸɬ@w(<&7|Ń=<6ɹ}Ň@ůŁ)|Ʊ <MOWf@Ʒ $)Ŀț<ɺŻǞǮ%,ɹ ËLjǕ)ǀɢ)ŃĊÓȎ(ƹƧM[jG8ɹǰǔǕ(} Š)đ$%<ȿɃ)đŀ<6)ɹ|6ȡǷ =ƫơ|õ8ªȠſ)9<Ʃ¼ö@nj$tracerǪ ƩŒŢũǫİ@Ƞoffline passive tracerhXk 3) ɷuɹ offlinehXk&àǩ<ɸ@nj<ɺofflinehXk,ș ţ+ƿƶ:+Ƴ®8ÝȾ4@ÚŴ)Ȍʼnɹ Ņ+îƿoŴµ))<tracer`iVIO+Ʃ¥('@ Ð;Ő&%<9)Ȥȡoŝȑ=$<ɺ3 ɹƫƘƩ¼&tracerȼɁ@ÚŴ)ȡǷ<onlineȡǷ& Ɣ1$ţÅ+Ƀ%ȡǷÓȎ%<&ɹȅŁ´nj )đ<þ(´ƿ<ɺŻǞǮ%,ɹofflinehXk +ɍnjłɹǂLjljø+Ǔ(<ƫò&+¯Ţǹè8ȼɁ ǃł+ĆǸúÁɹ)9/=:+gH\Pf@ţǕ) ƇȢoȦ<&@ǖǕ&<ɺtracer+Ńş®ƶ &$,ɹÇɜəłƫò%<ƽŌ©ƫȚɏ+|ƾ) ɫ<äéɩ¸oũËĄ¸ǔɩŎɹɵƺ+ĸɬ@ĵ Ñ<ɝşłƫě%<ÿĨƤƠěɌġƾ)ɫyɏ ɩ¸oƪęËĄ¸ǔɩŎ+2nŎ@Ð;t<ɺxËǔ ))<vʼn+}Š,ɹīĝɹǣŌɹþɠɹŽ('+ þɑĥê)ýþ(ĸɬ@Ì2ÓȎł; 2) ɹůŁ( }¶AQOgmYŸ3=$<ɺ 2. ,'.½ ŻǞǮ%,ɹJCOPE2ƫƤªȠſXpT 4) ɷƘĨȠ¢ĭ ǿ10 kmɸ@ŵüøǐż)9/±Źż&ɹɮ òƫƤļljhXkROMS@cpO&<1-way offline 2Ɠ ]OWBmJƫƤhXk®¸ 5-7) @Ʃ¼XpT&$nj <ɺđȮƫò+Ʃ¼+ªLJłȑā%<&,ū)Ǡ Ȩ=$< 5-7) ɺƽŌ©ƫ¦òƩ¼hXk 5, 6) %,ƘĨȠ ¢ĭ2 km+ROMSL1600 m+ROMS-L2S-1ɹ »-1ɸɹɌġƾƠěòƩ¼hXk 7) %,ROMSL1ɷƘ ĨȠ¢ĭ3 kmɸ:L2ɷÚ1 kmɸ0&UDmOKpj mJ@ȕɷS-2ɹ»-2ɸɹ==ROMSL2ɮò@

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, 60 ,2016 2

`

SEASONAL VARIABILITY OF LAND-DERIVED PASSIVE TRACER DISPERSAL IN THE SETO INLAND SEA AND THE ENSHU-NADA COAST

1 2 2 Yusuke UCHIYAMA, Yota SUZUE and Taichi KOSAKO

1 657-8501 1-1

2 657-8501 1-1

Coastal marginal seas and estuaries are generally dumpsites for wastewater from sewage and power plants. For an urgent assessment of dilution and dispersal of toxic materials due to accidental leakage, we develop an offline passive tracer model by exploiting oceanic reanalysis products and analyze differences in spatiotemporal variability of the leaked tracers in an estuary and a continental shelf margin on the Pacific side of Japan. In the estuary, the northeastward through flow affects the dispersal, while the month-long transport is dominated rather by inter-seasonal variability of wind-driven Ekman flow and counter-clockwise local circulations associated with the cold-dome density structure. On the marginal coast, the Kuroshio and resultant secondary recirculation readily entrain the tracer, leading to immediate transport mostly in the alongshore direction. The seasonal difference in the tracer dispersal is apparent such as sporadic offshore tracer eruption episodes, depending on the locations of the Kuroshio path.

Key Words : ROMS, coastal dispersal, offline Eulerian passive tracer model, Kuroshio, Seto Inland Sea

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monthly) 768) 1263) 1214) 54.6)max) 908) 1310) 1820) 63.9)mean) 264) 312) 717) 10.7)

East)138.84oE)

monthly) 313) 39.3) 411) 734)max) 313) 39.3) 411) 755)mean) 31.4) 9.21) 28.6) 184)

South)33.0)oN)

monthly) ND) ND) 445) 662)max) ND) ND) 640) 662)mean) ND) ND) 48.4) 191)

Suruga)Bay)

monthly) 372) 222) 57.0) 1291)max) 1258) 2029) 108) 1831)mean) 367) 666) 27.3) 1159)

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monthly) 0.15) 43.9) 56.4) ND)max) 0.15) 43.9) 56.4) ND)mean) 0.02) 5.45) 14.0) ND)

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1) Uchiyama, Y., Idica, E., McWilliams, J.C. and Stolzenbach, K.D.: Wastewater effluent dispersal in Southern California Bays, Cont. Shelf Res., No. 76, pp. 36-52, 2014.

2) 137

B2 Vol.68, No. 2, pp. I_931-I_935, 2012.

3) Idica, E. Y.: Contaminant Transport in the Southern California Bight, Ph.D. Dissertation, UCLA, 154 p., 2010.

4) Miyazawa, Y. and coauthors: Water mass variability in the western North Pacific detected in a 15-year eddy resolving ocean reanalysis. J. Oceanogr., Vol. 65, pp. 737-756, 2009.

5)

B2 , No. 68, Vol. 2, pp. I_441-I_445, 2012.

6) B3

, Vol. 71, No. 2, pp. I_383-I_388, 2015. 7)

) Argo 3,

B3 , Vol.71, No.2, pp. I_365-I_370, 2015. 8)

, B2 , Vol.71, No.2, pp. I_1231-

I_1236, 2015. 9) Chang, P.-H., Guo, X., and Takeoka, H.: A numerical study on

the seasonal circulation in the Seto Inland Sea, Japan. J. Oceanogr., Vol. 65, pp. 721-736, 2009.

2015.9.30