Fukushima-derived radiocesium in the western North Pacific in 2014
Abstract In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity concentration of Fukushima-derived radiocesium in surface mixed layer in 2012 had been transported eastward by 2014. In the south of the front we found...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kumamoto, Yuichiro [verfasserIn] Aoyama, Michio [verfasserIn] Hamajima, Yasunori [verfasserIn] Nagai, Hisao [verfasserIn] Yamagata, Takeyasu [verfasserIn] Kawai, Yoshimi [verfasserIn] Oka, Eitarou [verfasserIn] Yamaguchi, Atsushi [verfasserIn] Imai, Keiri [verfasserIn] Murata, Akihiko [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Journal of radioanalytical and nuclear chemistry - Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968, 311(2016), 2 vom: 03. Okt., Seite 1209-1217 |
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| Übergeordnetes Werk: |
volume:311 ; year:2016 ; number:2 ; day:03 ; month:10 ; pages:1209-1217 |
| Links: |
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| DOI / URN: |
10.1007/s10967-016-5055-3 |
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| Katalog-ID: |
SPR015213471 |
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| 520 | |a Abstract In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity concentration of Fukushima-derived radiocesium in surface mixed layer in 2012 had been transported eastward by 2014. In the south of the front we found a radiocesium subsurface maximum in 200–600 m depth, which was similar to that observed in 2012. The subsurface maximum spread southward from 18°N to 15°N between 2012 and 2014, which suggests spreading of Fukushima-derived radiocesium into the whole western subtropical area by 2014 due to formation and subduction of the subtropical mode water. | ||
| 650 | 4 | |a Fukushima Dai-ichi nuclear power plant accident |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Radiocesium |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a North Pacific Ocean |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Aoyama, Michio |e verfasserin |4 aut | |
| 700 | 1 | |a Hamajima, Yasunori |e verfasserin |4 aut | |
| 700 | 1 | |a Nagai, Hisao |e verfasserin |4 aut | |
| 700 | 1 | |a Yamagata, Takeyasu |e verfasserin |4 aut | |
| 700 | 1 | |a Kawai, Yoshimi |e verfasserin |4 aut | |
| 700 | 1 | |a Oka, Eitarou |e verfasserin |4 aut | |
| 700 | 1 | |a Yamaguchi, Atsushi |e verfasserin |4 aut | |
| 700 | 1 | |a Imai, Keiri |e verfasserin |4 aut | |
| 700 | 1 | |a Murata, Akihiko |e verfasserin |4 aut | |
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10.1007/s10967-016-5055-3 doi (DE-627)SPR015213471 (SPR)s10967-016-5055-3-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Kumamoto, Yuichiro verfasserin aut Fukushima-derived radiocesium in the western North Pacific in 2014 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity concentration of Fukushima-derived radiocesium in surface mixed layer in 2012 had been transported eastward by 2014. In the south of the front we found a radiocesium subsurface maximum in 200–600 m depth, which was similar to that observed in 2012. The subsurface maximum spread southward from 18°N to 15°N between 2012 and 2014, which suggests spreading of Fukushima-derived radiocesium into the whole western subtropical area by 2014 due to formation and subduction of the subtropical mode water. Fukushima Dai-ichi nuclear power plant accident (dpeaa)DE-He213 Radiocesium (dpeaa)DE-He213 North Pacific Ocean (dpeaa)DE-He213 Aoyama, Michio verfasserin aut Hamajima, Yasunori verfasserin aut Nagai, Hisao verfasserin aut Yamagata, Takeyasu verfasserin aut Kawai, Yoshimi verfasserin aut Oka, Eitarou verfasserin aut Yamaguchi, Atsushi verfasserin aut Imai, Keiri verfasserin aut Murata, Akihiko verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 311(2016), 2 vom: 03. Okt., Seite 1209-1217 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:311 year:2016 number:2 day:03 month:10 pages:1209-1217 https://dx.doi.org/10.1007/s10967-016-5055-3 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 311 2016 2 03 10 1209-1217 |
| spelling |
10.1007/s10967-016-5055-3 doi (DE-627)SPR015213471 (SPR)s10967-016-5055-3-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Kumamoto, Yuichiro verfasserin aut Fukushima-derived radiocesium in the western North Pacific in 2014 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity concentration of Fukushima-derived radiocesium in surface mixed layer in 2012 had been transported eastward by 2014. In the south of the front we found a radiocesium subsurface maximum in 200–600 m depth, which was similar to that observed in 2012. The subsurface maximum spread southward from 18°N to 15°N between 2012 and 2014, which suggests spreading of Fukushima-derived radiocesium into the whole western subtropical area by 2014 due to formation and subduction of the subtropical mode water. Fukushima Dai-ichi nuclear power plant accident (dpeaa)DE-He213 Radiocesium (dpeaa)DE-He213 North Pacific Ocean (dpeaa)DE-He213 Aoyama, Michio verfasserin aut Hamajima, Yasunori verfasserin aut Nagai, Hisao verfasserin aut Yamagata, Takeyasu verfasserin aut Kawai, Yoshimi verfasserin aut Oka, Eitarou verfasserin aut Yamaguchi, Atsushi verfasserin aut Imai, Keiri verfasserin aut Murata, Akihiko verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 311(2016), 2 vom: 03. Okt., Seite 1209-1217 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:311 year:2016 number:2 day:03 month:10 pages:1209-1217 https://dx.doi.org/10.1007/s10967-016-5055-3 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 311 2016 2 03 10 1209-1217 |
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10.1007/s10967-016-5055-3 doi (DE-627)SPR015213471 (SPR)s10967-016-5055-3-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Kumamoto, Yuichiro verfasserin aut Fukushima-derived radiocesium in the western North Pacific in 2014 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity concentration of Fukushima-derived radiocesium in surface mixed layer in 2012 had been transported eastward by 2014. In the south of the front we found a radiocesium subsurface maximum in 200–600 m depth, which was similar to that observed in 2012. The subsurface maximum spread southward from 18°N to 15°N between 2012 and 2014, which suggests spreading of Fukushima-derived radiocesium into the whole western subtropical area by 2014 due to formation and subduction of the subtropical mode water. Fukushima Dai-ichi nuclear power plant accident (dpeaa)DE-He213 Radiocesium (dpeaa)DE-He213 North Pacific Ocean (dpeaa)DE-He213 Aoyama, Michio verfasserin aut Hamajima, Yasunori verfasserin aut Nagai, Hisao verfasserin aut Yamagata, Takeyasu verfasserin aut Kawai, Yoshimi verfasserin aut Oka, Eitarou verfasserin aut Yamaguchi, Atsushi verfasserin aut Imai, Keiri verfasserin aut Murata, Akihiko verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 311(2016), 2 vom: 03. Okt., Seite 1209-1217 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:311 year:2016 number:2 day:03 month:10 pages:1209-1217 https://dx.doi.org/10.1007/s10967-016-5055-3 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 311 2016 2 03 10 1209-1217 |
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10.1007/s10967-016-5055-3 doi (DE-627)SPR015213471 (SPR)s10967-016-5055-3-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Kumamoto, Yuichiro verfasserin aut Fukushima-derived radiocesium in the western North Pacific in 2014 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity concentration of Fukushima-derived radiocesium in surface mixed layer in 2012 had been transported eastward by 2014. In the south of the front we found a radiocesium subsurface maximum in 200–600 m depth, which was similar to that observed in 2012. The subsurface maximum spread southward from 18°N to 15°N between 2012 and 2014, which suggests spreading of Fukushima-derived radiocesium into the whole western subtropical area by 2014 due to formation and subduction of the subtropical mode water. Fukushima Dai-ichi nuclear power plant accident (dpeaa)DE-He213 Radiocesium (dpeaa)DE-He213 North Pacific Ocean (dpeaa)DE-He213 Aoyama, Michio verfasserin aut Hamajima, Yasunori verfasserin aut Nagai, Hisao verfasserin aut Yamagata, Takeyasu verfasserin aut Kawai, Yoshimi verfasserin aut Oka, Eitarou verfasserin aut Yamaguchi, Atsushi verfasserin aut Imai, Keiri verfasserin aut Murata, Akihiko verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 311(2016), 2 vom: 03. Okt., Seite 1209-1217 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:311 year:2016 number:2 day:03 month:10 pages:1209-1217 https://dx.doi.org/10.1007/s10967-016-5055-3 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 311 2016 2 03 10 1209-1217 |
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10.1007/s10967-016-5055-3 doi (DE-627)SPR015213471 (SPR)s10967-016-5055-3-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Kumamoto, Yuichiro verfasserin aut Fukushima-derived radiocesium in the western North Pacific in 2014 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity concentration of Fukushima-derived radiocesium in surface mixed layer in 2012 had been transported eastward by 2014. In the south of the front we found a radiocesium subsurface maximum in 200–600 m depth, which was similar to that observed in 2012. The subsurface maximum spread southward from 18°N to 15°N between 2012 and 2014, which suggests spreading of Fukushima-derived radiocesium into the whole western subtropical area by 2014 due to formation and subduction of the subtropical mode water. Fukushima Dai-ichi nuclear power plant accident (dpeaa)DE-He213 Radiocesium (dpeaa)DE-He213 North Pacific Ocean (dpeaa)DE-He213 Aoyama, Michio verfasserin aut Hamajima, Yasunori verfasserin aut Nagai, Hisao verfasserin aut Yamagata, Takeyasu verfasserin aut Kawai, Yoshimi verfasserin aut Oka, Eitarou verfasserin aut Yamaguchi, Atsushi verfasserin aut Imai, Keiri verfasserin aut Murata, Akihiko verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 311(2016), 2 vom: 03. Okt., Seite 1209-1217 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:311 year:2016 number:2 day:03 month:10 pages:1209-1217 https://dx.doi.org/10.1007/s10967-016-5055-3 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 311 2016 2 03 10 1209-1217 |
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Kumamoto, Yuichiro @@aut@@ Aoyama, Michio @@aut@@ Hamajima, Yasunori @@aut@@ Nagai, Hisao @@aut@@ Yamagata, Takeyasu @@aut@@ Kawai, Yoshimi @@aut@@ Oka, Eitarou @@aut@@ Yamaguchi, Atsushi @@aut@@ Imai, Keiri @@aut@@ Murata, Akihiko @@aut@@ |
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Kumamoto, Yuichiro |
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Kumamoto, Yuichiro ddc 540 bkl 35.00 misc Fukushima Dai-ichi nuclear power plant accident misc Radiocesium misc North Pacific Ocean Fukushima-derived radiocesium in the western North Pacific in 2014 |
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540 ASE 35.00 bkl Fukushima-derived radiocesium in the western North Pacific in 2014 Fukushima Dai-ichi nuclear power plant accident (dpeaa)DE-He213 Radiocesium (dpeaa)DE-He213 North Pacific Ocean (dpeaa)DE-He213 |
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ddc 540 bkl 35.00 misc Fukushima Dai-ichi nuclear power plant accident misc Radiocesium misc North Pacific Ocean |
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ddc 540 bkl 35.00 misc Fukushima Dai-ichi nuclear power plant accident misc Radiocesium misc North Pacific Ocean |
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Fukushima-derived radiocesium in the western North Pacific in 2014 |
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Fukushima-derived radiocesium in the western North Pacific in 2014 |
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Kumamoto, Yuichiro |
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Kumamoto, Yuichiro Aoyama, Michio Hamajima, Yasunori Nagai, Hisao Yamagata, Takeyasu Kawai, Yoshimi Oka, Eitarou Yamaguchi, Atsushi Imai, Keiri Murata, Akihiko |
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540 ASE 35.00 bkl |
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fukushima-derived radiocesium in the western north pacific in 2014 |
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Fukushima-derived radiocesium in the western North Pacific in 2014 |
| abstract |
Abstract In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity concentration of Fukushima-derived radiocesium in surface mixed layer in 2012 had been transported eastward by 2014. In the south of the front we found a radiocesium subsurface maximum in 200–600 m depth, which was similar to that observed in 2012. The subsurface maximum spread southward from 18°N to 15°N between 2012 and 2014, which suggests spreading of Fukushima-derived radiocesium into the whole western subtropical area by 2014 due to formation and subduction of the subtropical mode water. |
| abstractGer |
Abstract In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity concentration of Fukushima-derived radiocesium in surface mixed layer in 2012 had been transported eastward by 2014. In the south of the front we found a radiocesium subsurface maximum in 200–600 m depth, which was similar to that observed in 2012. The subsurface maximum spread southward from 18°N to 15°N between 2012 and 2014, which suggests spreading of Fukushima-derived radiocesium into the whole western subtropical area by 2014 due to formation and subduction of the subtropical mode water. |
| abstract_unstemmed |
Abstract In 2014, we measured activity concentration of radiocesium in the western North Pacific Ocean. In the north of Kuroshio Front high activity concentration of Fukushima-derived radiocesium in surface mixed layer in 2012 had been transported eastward by 2014. In the south of the front we found a radiocesium subsurface maximum in 200–600 m depth, which was similar to that observed in 2012. The subsurface maximum spread southward from 18°N to 15°N between 2012 and 2014, which suggests spreading of Fukushima-derived radiocesium into the whole western subtropical area by 2014 due to formation and subduction of the subtropical mode water. |
| collection_details |
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| container_issue |
2 |
| title_short |
Fukushima-derived radiocesium in the western North Pacific in 2014 |
| url |
https://dx.doi.org/10.1007/s10967-016-5055-3 |
| remote_bool |
true |
| author2 |
Aoyama, Michio Hamajima, Yasunori Nagai, Hisao Yamagata, Takeyasu Kawai, Yoshimi Oka, Eitarou Yamaguchi, Atsushi Imai, Keiri Murata, Akihiko |
| author2Str |
Aoyama, Michio Hamajima, Yasunori Nagai, Hisao Yamagata, Takeyasu Kawai, Yoshimi Oka, Eitarou Yamaguchi, Atsushi Imai, Keiri Murata, Akihiko |
| ppnlink |
320578011 |
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c |
| isOA_txt |
true |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/s10967-016-5055-3 |
| up_date |
2024-07-03T14:41:56.598Z |
| _version_ |
1803569297204707328 |
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| score |
7.401758 |