Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean

Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic b...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Xiaoxia Cai [verfasserIn] Yanpei Zhuang [verfasserIn] Hongliang Li [verfasserIn] Jing Xu [verfasserIn] Haiyan Jin [verfasserIn] Jianfang Chen [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Schlagwörter:	colored DOM marine carbon cycle Arctic Ocean ice melt Pacific water inflow

Übergeordnetes Werk:	In: Journal of Marine Science and Engineering - MDPI AG, 2014, 10(2022), 3, p 352
Übergeordnetes Werk:	volume:10 ; year:2022 ; number:3, p 352

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/jmse10030352

Katalog-ID:	DOAJ04779576X

Internformat


LEADER	01000caa a22002652 4500
001	DOAJ04779576X
003	DE-627
005	20240414174038.0
007	cr uuu---uuuuu
008	230227s2022 xx \|\|\|\|\|o 00\| \|\|eng c
024	7		\|a 10.3390/jmse10030352 \|2 doi
035			\|a (DE-627)DOAJ04779576X
035			\|a (DE-599)DOAJfe1fc42979c94ac1bb39a485906373b3
040			\|a DE-627 \|b ger \|c DE-627 \|e rakwb
041			\|a eng
050		0	\|a VM1-989
050		0	\|a GC1-1581
100	0		\|a Xiaoxia Cai \|e verfasserin \|4 aut
245	1	0	\|a Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean
264		1	\|c 2022
336			\|a Text \|b txt \|2 rdacontent
337			\|a Computermedien \|b c \|2 rdamedia
338			\|a Online-Ressource \|b cr \|2 rdacarrier
520			\|a Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean.
650		4	\|a colored DOM
650		4	\|a marine carbon cycle
650		4	\|a Arctic Ocean
650		4	\|a ice melt
650		4	\|a Pacific water inflow
653		0	\|a Naval architecture. Shipbuilding. Marine engineering
653		0	\|a Oceanography
700	0		\|a Yanpei Zhuang \|e verfasserin \|4 aut
700	0		\|a Hongliang Li \|e verfasserin \|4 aut
700	0		\|a Jing Xu \|e verfasserin \|4 aut
700	0		\|a Haiyan Jin \|e verfasserin \|4 aut
700	0		\|a Jianfang Chen \|e verfasserin \|4 aut
773	0	8	\|i In \|t Journal of Marine Science and Engineering \|d MDPI AG, 2014 \|g 10(2022), 3, p 352 \|w (DE-627)771274181 \|w (DE-600)2738390-8 \|x 20771312 \|7 nnns
773	1	8	\|g volume:10 \|g year:2022 \|g number:3, p 352
856	4	0	\|u https://doi.org/10.3390/jmse10030352 \|z kostenfrei
856	4	0	\|u https://doaj.org/article/fe1fc42979c94ac1bb39a485906373b3 \|z kostenfrei
856	4	0	\|u https://www.mdpi.com/2077-1312/10/3/352 \|z kostenfrei
856	4	2	\|u https://doaj.org/toc/2077-1312 \|y Journal toc \|z kostenfrei
912			\|a GBV_USEFLAG_A
912			\|a SYSFLAG_A
912			\|a GBV_DOAJ
912			\|a GBV_ILN_11
912			\|a GBV_ILN_20
912			\|a GBV_ILN_22
912			\|a GBV_ILN_23
912			\|a GBV_ILN_24
912			\|a GBV_ILN_39
912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_65
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_95
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_151
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_213
912			\|a GBV_ILN_230
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_4012
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4249
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4306
912			\|a GBV_ILN_4307
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4325
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4338
912			\|a GBV_ILN_4367
912			\|a GBV_ILN_4700
951			\|a AR
952			\|d 10 \|j 2022 \|e 3, p 352

Indexfelder

author_variant	x c xc y z yz h l hl j x jx h j hj j c jc
matchkey_str	article:20771312:2022----::ptadsrbtooclrdisleogncatrnh
hierarchy_sort_str	2022
callnumber-subject-code	VM
publishDate	2022
allfields	10.3390/jmse10030352 doi (DE-627)DOAJ04779576X (DE-599)DOAJfe1fc42979c94ac1bb39a485906373b3 DE-627 ger DE-627 rakwb eng VM1-989 GC1-1581 Xiaoxia Cai verfasserin aut Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean. colored DOM marine carbon cycle Arctic Ocean ice melt Pacific water inflow Naval architecture. Shipbuilding. Marine engineering Oceanography Yanpei Zhuang verfasserin aut Hongliang Li verfasserin aut Jing Xu verfasserin aut Haiyan Jin verfasserin aut Jianfang Chen verfasserin aut In Journal of Marine Science and Engineering MDPI AG, 2014 10(2022), 3, p 352 (DE-627)771274181 (DE-600)2738390-8 20771312 nnns volume:10 year:2022 number:3, p 352 https://doi.org/10.3390/jmse10030352 kostenfrei https://doaj.org/article/fe1fc42979c94ac1bb39a485906373b3 kostenfrei https://www.mdpi.com/2077-1312/10/3/352 kostenfrei https://doaj.org/toc/2077-1312 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022 3, p 352
spelling	10.3390/jmse10030352 doi (DE-627)DOAJ04779576X (DE-599)DOAJfe1fc42979c94ac1bb39a485906373b3 DE-627 ger DE-627 rakwb eng VM1-989 GC1-1581 Xiaoxia Cai verfasserin aut Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean. colored DOM marine carbon cycle Arctic Ocean ice melt Pacific water inflow Naval architecture. Shipbuilding. Marine engineering Oceanography Yanpei Zhuang verfasserin aut Hongliang Li verfasserin aut Jing Xu verfasserin aut Haiyan Jin verfasserin aut Jianfang Chen verfasserin aut In Journal of Marine Science and Engineering MDPI AG, 2014 10(2022), 3, p 352 (DE-627)771274181 (DE-600)2738390-8 20771312 nnns volume:10 year:2022 number:3, p 352 https://doi.org/10.3390/jmse10030352 kostenfrei https://doaj.org/article/fe1fc42979c94ac1bb39a485906373b3 kostenfrei https://www.mdpi.com/2077-1312/10/3/352 kostenfrei https://doaj.org/toc/2077-1312 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022 3, p 352
allfields_unstemmed	10.3390/jmse10030352 doi (DE-627)DOAJ04779576X (DE-599)DOAJfe1fc42979c94ac1bb39a485906373b3 DE-627 ger DE-627 rakwb eng VM1-989 GC1-1581 Xiaoxia Cai verfasserin aut Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean. colored DOM marine carbon cycle Arctic Ocean ice melt Pacific water inflow Naval architecture. Shipbuilding. Marine engineering Oceanography Yanpei Zhuang verfasserin aut Hongliang Li verfasserin aut Jing Xu verfasserin aut Haiyan Jin verfasserin aut Jianfang Chen verfasserin aut In Journal of Marine Science and Engineering MDPI AG, 2014 10(2022), 3, p 352 (DE-627)771274181 (DE-600)2738390-8 20771312 nnns volume:10 year:2022 number:3, p 352 https://doi.org/10.3390/jmse10030352 kostenfrei https://doaj.org/article/fe1fc42979c94ac1bb39a485906373b3 kostenfrei https://www.mdpi.com/2077-1312/10/3/352 kostenfrei https://doaj.org/toc/2077-1312 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022 3, p 352
allfieldsGer	10.3390/jmse10030352 doi (DE-627)DOAJ04779576X (DE-599)DOAJfe1fc42979c94ac1bb39a485906373b3 DE-627 ger DE-627 rakwb eng VM1-989 GC1-1581 Xiaoxia Cai verfasserin aut Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean. colored DOM marine carbon cycle Arctic Ocean ice melt Pacific water inflow Naval architecture. Shipbuilding. Marine engineering Oceanography Yanpei Zhuang verfasserin aut Hongliang Li verfasserin aut Jing Xu verfasserin aut Haiyan Jin verfasserin aut Jianfang Chen verfasserin aut In Journal of Marine Science and Engineering MDPI AG, 2014 10(2022), 3, p 352 (DE-627)771274181 (DE-600)2738390-8 20771312 nnns volume:10 year:2022 number:3, p 352 https://doi.org/10.3390/jmse10030352 kostenfrei https://doaj.org/article/fe1fc42979c94ac1bb39a485906373b3 kostenfrei https://www.mdpi.com/2077-1312/10/3/352 kostenfrei https://doaj.org/toc/2077-1312 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022 3, p 352
allfieldsSound	10.3390/jmse10030352 doi (DE-627)DOAJ04779576X (DE-599)DOAJfe1fc42979c94ac1bb39a485906373b3 DE-627 ger DE-627 rakwb eng VM1-989 GC1-1581 Xiaoxia Cai verfasserin aut Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean. colored DOM marine carbon cycle Arctic Ocean ice melt Pacific water inflow Naval architecture. Shipbuilding. Marine engineering Oceanography Yanpei Zhuang verfasserin aut Hongliang Li verfasserin aut Jing Xu verfasserin aut Haiyan Jin verfasserin aut Jianfang Chen verfasserin aut In Journal of Marine Science and Engineering MDPI AG, 2014 10(2022), 3, p 352 (DE-627)771274181 (DE-600)2738390-8 20771312 nnns volume:10 year:2022 number:3, p 352 https://doi.org/10.3390/jmse10030352 kostenfrei https://doaj.org/article/fe1fc42979c94ac1bb39a485906373b3 kostenfrei https://www.mdpi.com/2077-1312/10/3/352 kostenfrei https://doaj.org/toc/2077-1312 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022 3, p 352
language	English
source	In Journal of Marine Science and Engineering 10(2022), 3, p 352 volume:10 year:2022 number:3, p 352
sourceStr	In Journal of Marine Science and Engineering 10(2022), 3, p 352 volume:10 year:2022 number:3, p 352
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	colored DOM marine carbon cycle Arctic Ocean ice melt Pacific water inflow Naval architecture. Shipbuilding. Marine engineering Oceanography
isfreeaccess_bool	true
container_title	Journal of Marine Science and Engineering
authorswithroles_txt_mv	Xiaoxia Cai @@aut@@ Yanpei Zhuang @@aut@@ Hongliang Li @@aut@@ Jing Xu @@aut@@ Haiyan Jin @@aut@@ Jianfang Chen @@aut@@
publishDateDaySort_date	2022-01-01T00:00:00Z
hierarchy_top_id	771274181
id	DOAJ04779576X
language_de	englisch
fullrecord	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">DOAJ04779576X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240414174038.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230227s2022 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.3390/jmse10030352</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ04779576X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJfe1fc42979c94ac1bb39a485906373b3</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="050" ind1=" " ind2="0"><subfield code="a">VM1-989</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">GC1-1581</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Xiaoxia Cai</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</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">Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">colored DOM</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">marine carbon cycle</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Arctic Ocean</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">ice melt</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pacific water inflow</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Naval architecture. Shipbuilding. Marine engineering</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Oceanography</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Yanpei Zhuang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Hongliang Li</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Jing Xu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Haiyan Jin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Jianfang Chen</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Journal of Marine Science and Engineering</subfield><subfield code="d">MDPI AG, 2014</subfield><subfield code="g">10(2022), 3, p 352</subfield><subfield code="w">(DE-627)771274181</subfield><subfield code="w">(DE-600)2738390-8</subfield><subfield code="x">20771312</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:10</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:3, p 352</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.3390/jmse10030352</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/fe1fc42979c94ac1bb39a485906373b3</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://www.mdpi.com/2077-1312/10/3/352</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2077-1312</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</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_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4367</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">10</subfield><subfield code="j">2022</subfield><subfield code="e">3, p 352</subfield></datafield></record></collection>
callnumber-first	V - Naval Science
author	Xiaoxia Cai
spellingShingle	Xiaoxia Cai misc VM1-989 misc GC1-1581 misc colored DOM misc marine carbon cycle misc Arctic Ocean misc ice melt misc Pacific water inflow misc Naval architecture. Shipbuilding. Marine engineering misc Oceanography Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean
authorStr	Xiaoxia Cai
ppnlink_with_tag_str_mv	@@773@@(DE-627)771274181
format	electronic Article
delete_txt_mv	keep
author_role	aut aut aut aut aut aut
collection	DOAJ
remote_str	true
callnumber-label	VM1-989
illustrated	Not Illustrated
issn	20771312
topic_title	VM1-989 GC1-1581 Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean colored DOM marine carbon cycle Arctic Ocean ice melt Pacific water inflow
topic	misc VM1-989 misc GC1-1581 misc colored DOM misc marine carbon cycle misc Arctic Ocean misc ice melt misc Pacific water inflow misc Naval architecture. Shipbuilding. Marine engineering misc Oceanography
topic_unstemmed	misc VM1-989 misc GC1-1581 misc colored DOM misc marine carbon cycle misc Arctic Ocean misc ice melt misc Pacific water inflow misc Naval architecture. Shipbuilding. Marine engineering misc Oceanography
topic_browse	misc VM1-989 misc GC1-1581 misc colored DOM misc marine carbon cycle misc Arctic Ocean misc ice melt misc Pacific water inflow misc Naval architecture. Shipbuilding. Marine engineering misc Oceanography
format_facet	Elektronische Aufsätze Aufsätze Elektronische Ressource
format_main_str_mv	Text Zeitschrift/Artikel
carriertype_str_mv	cr
hierarchy_parent_title	Journal of Marine Science and Engineering
hierarchy_parent_id	771274181
hierarchy_top_title	Journal of Marine Science and Engineering
isfreeaccess_txt	true
familylinks_str_mv	(DE-627)771274181 (DE-600)2738390-8
title	Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean
ctrlnum	(DE-627)DOAJ04779576X (DE-599)DOAJfe1fc42979c94ac1bb39a485906373b3
title_full	Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean
author_sort	Xiaoxia Cai
journal	Journal of Marine Science and Engineering
journalStr	Journal of Marine Science and Engineering
callnumber-first-code	V
lang_code	eng
isOA_bool	true
recordtype	marc
publishDateSort	2022
contenttype_str_mv	txt
author_browse	Xiaoxia Cai Yanpei Zhuang Hongliang Li Jing Xu Haiyan Jin Jianfang Chen
container_volume	10
class	VM1-989 GC1-1581
format_se	Elektronische Aufsätze
author-letter	Xiaoxia Cai
doi_str_mv	10.3390/jmse10030352
author2-role	verfasserin
title_sort	spatial distribution of colored dissolved organic matter in the western arctic ocean
callnumber	VM1-989
title_auth	Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean
abstract	Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean.
abstractGer	Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean.
abstract_unstemmed	Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean.
collection_details	GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700
container_issue	3, p 352
title_short	Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean
url	https://doi.org/10.3390/jmse10030352 https://doaj.org/article/fe1fc42979c94ac1bb39a485906373b3 https://www.mdpi.com/2077-1312/10/3/352 https://doaj.org/toc/2077-1312
remote_bool	true
author2	Yanpei Zhuang Hongliang Li Jing Xu Haiyan Jin Jianfang Chen
author2Str	Yanpei Zhuang Hongliang Li Jing Xu Haiyan Jin Jianfang Chen
ppnlink	771274181
callnumber-subject	VM - Naval Architecture, Shipbuilding, Marine Engineering
mediatype_str_mv	c
isOA_txt	true
hochschulschrift_bool	false
doi_str	10.3390/jmse10030352
callnumber-a	VM1-989
up_date	2024-07-03T14:11:13.786Z
_version_	1803567364881514496
fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">DOAJ04779576X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240414174038.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230227s2022 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.3390/jmse10030352</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ04779576X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJfe1fc42979c94ac1bb39a485906373b3</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="050" ind1=" " ind2="0"><subfield code="a">VM1-989</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">GC1-1581</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Xiaoxia Cai</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</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">Optical properties of colored dissolved organic matter (CDOM) were investigated along a latitudinal transect (67°–77° N) in upper water (<80 m depth) of the western Arctic Ocean. The absorption coefficient at 280 nm was 0.48–1.25 m<sup<−1</sup<, with the average for the oligotrophic basin area (1.04 ± 0.08 m<sup<−1</sup<) being slightly higher than that of the productive shelf area (0.95 ± 0.16 m<sup<−1</sup<), implying a decoupling effect between CDOM concentration and biological productivity in the western Arctic Ocean. The spectral slope coefficient <i<S</i<<sub<270–350</sub< was negatively correlated with salinity, indicating that DOM molecular weight increases with salinity, and may be affected by melt-water input. Four fluorescent components were identified by excitation emission matrices elaborated by parallel factor analysis, including three humic-like (C1, C3, and C4) components and one protein-like (C2) component. Significant increases in concentrations of terrestrially derived humic-like C3 and C4 components with salinity were observed in the basin, mainly controlled by the physical mixing of surface fresh water and subsurface inflowing Pacific Ocean water. Terrestrial material carried by Pacific inflow is thus an important factor affecting the distribution of CDOM fluorescence components. The C3 and C4 fluorescence components may be useful as tracers of Pacific water in the western Arctic Ocean.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">colored DOM</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">marine carbon cycle</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Arctic Ocean</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">ice melt</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Pacific water inflow</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Naval architecture. Shipbuilding. Marine engineering</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Oceanography</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Yanpei Zhuang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Hongliang Li</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Jing Xu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Haiyan Jin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Jianfang Chen</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Journal of Marine Science and Engineering</subfield><subfield code="d">MDPI AG, 2014</subfield><subfield code="g">10(2022), 3, p 352</subfield><subfield code="w">(DE-627)771274181</subfield><subfield code="w">(DE-600)2738390-8</subfield><subfield code="x">20771312</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:10</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:3, p 352</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.3390/jmse10030352</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/fe1fc42979c94ac1bb39a485906373b3</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://www.mdpi.com/2077-1312/10/3/352</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2077-1312</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</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_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4367</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">10</subfield><subfield code="j">2022</subfield><subfield code="e">3, p 352</subfield></datafield></record></collection>
score	7.3993187

Nicht das Richtige dabei?

Schreiben Sie uns!

Spatial Distribution of Colored Dissolved Organic Matter in the Western Arctic Ocean

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?