Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions
Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST me...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kawai, Yoshimi [verfasserIn] Kawamura, Hiroshi [verfasserIn] Tanba, Sumio [verfasserIn] Ando, Kentaro [verfasserIn] Yoneyama, Kunio [verfasserIn] Nagahama, Norio [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2006 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Journal of oceanography - Dordrecht [u.a.] : Springer Science + Business Media B.V, 1942, 62(2006), 6 vom: 01. Dez., Seite 825-838 |
|---|---|
| Übergeordnetes Werk: |
volume:62 ; year:2006 ; number:6 ; day:01 ; month:12 ; pages:825-838 |
| Links: |
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| DOI / URN: |
10.1007/s10872-006-0101-3 |
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| Katalog-ID: |
SPR014221136 |
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| 245 | 1 | 0 | |a Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions |
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| 520 | |a Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST ($ SST_{1.5m} $) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the $ SST_{1.5m} $ in these cases could not be accounted for by solar heating alone. We examined the depth of the $ SST_{1.5m} $ sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the $ SST_{1.5m} $ observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the $ SST_{1.5m} $ exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. A simple formula is proposed to correct the unexpected diurnal amplitude of the buoy $ SST_{1.5m} $. | ||
| 650 | 4 | |a SST |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a diurnal warming |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a platform effect |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a TRITON buoy |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a western tropical Pacific |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Kawamura, Hiroshi |e verfasserin |4 aut | |
| 700 | 1 | |a Tanba, Sumio |e verfasserin |4 aut | |
| 700 | 1 | |a Ando, Kentaro |e verfasserin |4 aut | |
| 700 | 1 | |a Yoneyama, Kunio |e verfasserin |4 aut | |
| 700 | 1 | |a Nagahama, Norio |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Journal of oceanography |d Dordrecht [u.a.] : Springer Science + Business Media B.V, 1942 |g 62(2006), 6 vom: 01. Dez., Seite 825-838 |w (DE-627)320575829 |w (DE-600)2017037-3 |x 1573-868X |7 nnns |
| 773 | 1 | 8 | |g volume:62 |g year:2006 |g number:6 |g day:01 |g month:12 |g pages:825-838 |
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10.1007/s10872-006-0101-3 doi (DE-627)SPR014221136 (SPR)s10872-006-0101-3-e DE-627 ger DE-627 rakwb eng 550 ASE 38.90 bkl Kawai, Yoshimi verfasserin aut Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST ($ SST_{1.5m} $) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the $ SST_{1.5m} $ in these cases could not be accounted for by solar heating alone. We examined the depth of the $ SST_{1.5m} $ sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the $ SST_{1.5m} $ observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the $ SST_{1.5m} $ exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. A simple formula is proposed to correct the unexpected diurnal amplitude of the buoy $ SST_{1.5m} $. SST (dpeaa)DE-He213 diurnal warming (dpeaa)DE-He213 platform effect (dpeaa)DE-He213 TRITON buoy (dpeaa)DE-He213 western tropical Pacific (dpeaa)DE-He213 Kawamura, Hiroshi verfasserin aut Tanba, Sumio verfasserin aut Ando, Kentaro verfasserin aut Yoneyama, Kunio verfasserin aut Nagahama, Norio verfasserin aut Enthalten in Journal of oceanography Dordrecht [u.a.] : Springer Science + Business Media B.V, 1942 62(2006), 6 vom: 01. Dez., Seite 825-838 (DE-627)320575829 (DE-600)2017037-3 1573-868X nnns volume:62 year:2006 number:6 day:01 month:12 pages:825-838 https://dx.doi.org/10.1007/s10872-006-0101-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 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_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_4367 GBV_ILN_4393 GBV_ILN_4700 38.90 ASE AR 62 2006 6 01 12 825-838 |
| spelling |
10.1007/s10872-006-0101-3 doi (DE-627)SPR014221136 (SPR)s10872-006-0101-3-e DE-627 ger DE-627 rakwb eng 550 ASE 38.90 bkl Kawai, Yoshimi verfasserin aut Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST ($ SST_{1.5m} $) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the $ SST_{1.5m} $ in these cases could not be accounted for by solar heating alone. We examined the depth of the $ SST_{1.5m} $ sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the $ SST_{1.5m} $ observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the $ SST_{1.5m} $ exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. A simple formula is proposed to correct the unexpected diurnal amplitude of the buoy $ SST_{1.5m} $. SST (dpeaa)DE-He213 diurnal warming (dpeaa)DE-He213 platform effect (dpeaa)DE-He213 TRITON buoy (dpeaa)DE-He213 western tropical Pacific (dpeaa)DE-He213 Kawamura, Hiroshi verfasserin aut Tanba, Sumio verfasserin aut Ando, Kentaro verfasserin aut Yoneyama, Kunio verfasserin aut Nagahama, Norio verfasserin aut Enthalten in Journal of oceanography Dordrecht [u.a.] : Springer Science + Business Media B.V, 1942 62(2006), 6 vom: 01. Dez., Seite 825-838 (DE-627)320575829 (DE-600)2017037-3 1573-868X nnns volume:62 year:2006 number:6 day:01 month:12 pages:825-838 https://dx.doi.org/10.1007/s10872-006-0101-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 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_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_4367 GBV_ILN_4393 GBV_ILN_4700 38.90 ASE AR 62 2006 6 01 12 825-838 |
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10.1007/s10872-006-0101-3 doi (DE-627)SPR014221136 (SPR)s10872-006-0101-3-e DE-627 ger DE-627 rakwb eng 550 ASE 38.90 bkl Kawai, Yoshimi verfasserin aut Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST ($ SST_{1.5m} $) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the $ SST_{1.5m} $ in these cases could not be accounted for by solar heating alone. We examined the depth of the $ SST_{1.5m} $ sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the $ SST_{1.5m} $ observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the $ SST_{1.5m} $ exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. A simple formula is proposed to correct the unexpected diurnal amplitude of the buoy $ SST_{1.5m} $. SST (dpeaa)DE-He213 diurnal warming (dpeaa)DE-He213 platform effect (dpeaa)DE-He213 TRITON buoy (dpeaa)DE-He213 western tropical Pacific (dpeaa)DE-He213 Kawamura, Hiroshi verfasserin aut Tanba, Sumio verfasserin aut Ando, Kentaro verfasserin aut Yoneyama, Kunio verfasserin aut Nagahama, Norio verfasserin aut Enthalten in Journal of oceanography Dordrecht [u.a.] : Springer Science + Business Media B.V, 1942 62(2006), 6 vom: 01. Dez., Seite 825-838 (DE-627)320575829 (DE-600)2017037-3 1573-868X nnns volume:62 year:2006 number:6 day:01 month:12 pages:825-838 https://dx.doi.org/10.1007/s10872-006-0101-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 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_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_4367 GBV_ILN_4393 GBV_ILN_4700 38.90 ASE AR 62 2006 6 01 12 825-838 |
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10.1007/s10872-006-0101-3 doi (DE-627)SPR014221136 (SPR)s10872-006-0101-3-e DE-627 ger DE-627 rakwb eng 550 ASE 38.90 bkl Kawai, Yoshimi verfasserin aut Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST ($ SST_{1.5m} $) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the $ SST_{1.5m} $ in these cases could not be accounted for by solar heating alone. We examined the depth of the $ SST_{1.5m} $ sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the $ SST_{1.5m} $ observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the $ SST_{1.5m} $ exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. A simple formula is proposed to correct the unexpected diurnal amplitude of the buoy $ SST_{1.5m} $. SST (dpeaa)DE-He213 diurnal warming (dpeaa)DE-He213 platform effect (dpeaa)DE-He213 TRITON buoy (dpeaa)DE-He213 western tropical Pacific (dpeaa)DE-He213 Kawamura, Hiroshi verfasserin aut Tanba, Sumio verfasserin aut Ando, Kentaro verfasserin aut Yoneyama, Kunio verfasserin aut Nagahama, Norio verfasserin aut Enthalten in Journal of oceanography Dordrecht [u.a.] : Springer Science + Business Media B.V, 1942 62(2006), 6 vom: 01. Dez., Seite 825-838 (DE-627)320575829 (DE-600)2017037-3 1573-868X nnns volume:62 year:2006 number:6 day:01 month:12 pages:825-838 https://dx.doi.org/10.1007/s10872-006-0101-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 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_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_4367 GBV_ILN_4393 GBV_ILN_4700 38.90 ASE AR 62 2006 6 01 12 825-838 |
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10.1007/s10872-006-0101-3 doi (DE-627)SPR014221136 (SPR)s10872-006-0101-3-e DE-627 ger DE-627 rakwb eng 550 ASE 38.90 bkl Kawai, Yoshimi verfasserin aut Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST ($ SST_{1.5m} $) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the $ SST_{1.5m} $ in these cases could not be accounted for by solar heating alone. We examined the depth of the $ SST_{1.5m} $ sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the $ SST_{1.5m} $ observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the $ SST_{1.5m} $ exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. A simple formula is proposed to correct the unexpected diurnal amplitude of the buoy $ SST_{1.5m} $. SST (dpeaa)DE-He213 diurnal warming (dpeaa)DE-He213 platform effect (dpeaa)DE-He213 TRITON buoy (dpeaa)DE-He213 western tropical Pacific (dpeaa)DE-He213 Kawamura, Hiroshi verfasserin aut Tanba, Sumio verfasserin aut Ando, Kentaro verfasserin aut Yoneyama, Kunio verfasserin aut Nagahama, Norio verfasserin aut Enthalten in Journal of oceanography Dordrecht [u.a.] : Springer Science + Business Media B.V, 1942 62(2006), 6 vom: 01. Dez., Seite 825-838 (DE-627)320575829 (DE-600)2017037-3 1573-868X nnns volume:62 year:2006 number:6 day:01 month:12 pages:825-838 https://dx.doi.org/10.1007/s10872-006-0101-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 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_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_4367 GBV_ILN_4393 GBV_ILN_4700 38.90 ASE AR 62 2006 6 01 12 825-838 |
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English |
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Enthalten in Journal of oceanography 62(2006), 6 vom: 01. Dez., Seite 825-838 volume:62 year:2006 number:6 day:01 month:12 pages:825-838 |
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Enthalten in Journal of oceanography 62(2006), 6 vom: 01. Dez., Seite 825-838 volume:62 year:2006 number:6 day:01 month:12 pages:825-838 |
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SST diurnal warming platform effect TRITON buoy western tropical Pacific |
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Journal of oceanography |
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Kawai, Yoshimi @@aut@@ Kawamura, Hiroshi @@aut@@ Tanba, Sumio @@aut@@ Ando, Kentaro @@aut@@ Yoneyama, Kunio @@aut@@ Nagahama, Norio @@aut@@ |
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2006-12-01T00:00:00Z |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR014221136</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220111005526.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201006s2006 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10872-006-0101-3</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR014221136</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s10872-006-0101-3-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.90</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Kawai, Yoshimi</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2006</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST ($ SST_{1.5m} $) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the $ SST_{1.5m} $ in these cases could not be accounted for by solar heating alone. We examined the depth of the $ SST_{1.5m} $ sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the $ SST_{1.5m} $ observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the $ SST_{1.5m} $ exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. 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Dez., Seite 825-838</subfield><subfield code="w">(DE-627)320575829</subfield><subfield code="w">(DE-600)2017037-3</subfield><subfield code="x">1573-868X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:62</subfield><subfield code="g">year:2006</subfield><subfield code="g">number:6</subfield><subfield code="g">day:01</subfield><subfield code="g">month:12</subfield><subfield code="g">pages:825-838</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s10872-006-0101-3</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" 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|
| author |
Kawai, Yoshimi |
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Kawai, Yoshimi ddc 550 bkl 38.90 misc SST misc diurnal warming misc platform effect misc TRITON buoy misc western tropical Pacific Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions |
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550 ASE 38.90 bkl Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions SST (dpeaa)DE-He213 diurnal warming (dpeaa)DE-He213 platform effect (dpeaa)DE-He213 TRITON buoy (dpeaa)DE-He213 western tropical Pacific (dpeaa)DE-He213 |
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ddc 550 bkl 38.90 misc SST misc diurnal warming misc platform effect misc TRITON buoy misc western tropical Pacific |
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ddc 550 bkl 38.90 misc SST misc diurnal warming misc platform effect misc TRITON buoy misc western tropical Pacific |
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Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions |
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Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions |
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Kawai, Yoshimi |
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Journal of oceanography |
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Kawai, Yoshimi Kawamura, Hiroshi Tanba, Sumio Ando, Kentaro Yoneyama, Kunio Nagahama, Norio |
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550 ASE 38.90 bkl |
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| title_sort |
validity of sea surface temperature observed with the triton buoy under diurnal heating conditions |
| title_auth |
Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions |
| abstract |
Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST ($ SST_{1.5m} $) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the $ SST_{1.5m} $ in these cases could not be accounted for by solar heating alone. We examined the depth of the $ SST_{1.5m} $ sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the $ SST_{1.5m} $ observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the $ SST_{1.5m} $ exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. A simple formula is proposed to correct the unexpected diurnal amplitude of the buoy $ SST_{1.5m} $. |
| abstractGer |
Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST ($ SST_{1.5m} $) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the $ SST_{1.5m} $ in these cases could not be accounted for by solar heating alone. We examined the depth of the $ SST_{1.5m} $ sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the $ SST_{1.5m} $ observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the $ SST_{1.5m} $ exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. A simple formula is proposed to correct the unexpected diurnal amplitude of the buoy $ SST_{1.5m} $. |
| abstract_unstemmed |
Abstract In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST ($ SST_{1.5m} $) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the $ SST_{1.5m} $ in these cases could not be accounted for by solar heating alone. We examined the depth of the $ SST_{1.5m} $ sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the $ SST_{1.5m} $ observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the $ SST_{1.5m} $ exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. A simple formula is proposed to correct the unexpected diurnal amplitude of the buoy $ SST_{1.5m} $. |
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6 |
| title_short |
Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions |
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https://dx.doi.org/10.1007/s10872-006-0101-3 |
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Kawamura, Hiroshi Tanba, Sumio Ando, Kentaro Yoneyama, Kunio Nagahama, Norio |
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Kawamura, Hiroshi Tanba, Sumio Ando, Kentaro Yoneyama, Kunio Nagahama, Norio |
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10.1007/s10872-006-0101-3 |
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2024-07-04T00:42:07.732Z |
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| score |
7.401785 |