An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea
Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net pri...
Ausführliche Beschreibung
Autor*in: |
Hahm, Doshik [verfasserIn] |
---|
Format: |
E-Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2019transfer abstract |
---|
Umfang: |
8 |
---|
Übergeordnetes Werk: |
Enthalten in: Investigating the urban heat island effect of transit oriented development in Brisbane - Kamruzzaman, Md. ELSEVIER, 2017, New York, NY [u.a.] |
---|---|
Übergeordnetes Werk: |
volume:195 ; year:2019 ; pages:30-37 ; extent:8 |
Links: |
---|
DOI / URN: |
10.1016/j.jmarsys.2019.03.005 |
---|
Katalog-ID: |
ELV046518304 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | ELV046518304 | ||
003 | DE-627 | ||
005 | 20230626013837.0 | ||
007 | cr uuu---uuuuu | ||
008 | 191021s2019 xx |||||o 00| ||eng c | ||
024 | 7 | |a 10.1016/j.jmarsys.2019.03.005 |2 doi | |
028 | 5 | 2 | |a GBV00000000000613.pica |
035 | |a (DE-627)ELV046518304 | ||
035 | |a (ELSEVIER)S0924-7963(18)30279-3 | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 380 |a 910 |q VZ |
084 | |a 55.80 |2 bkl | ||
084 | |a 74.08 |2 bkl | ||
084 | |a 74.75 |2 bkl | ||
100 | 1 | |a Hahm, Doshik |e verfasserin |4 aut | |
245 | 1 | 0 | |a An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea |
264 | 1 | |c 2019transfer abstract | |
300 | |a 8 | ||
336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
337 | |a nicht spezifiziert |b z |2 rdamedia | ||
338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
520 | |a Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. | ||
520 | |a Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. | ||
700 | 1 | |a Rhee, Tae Siek |4 oth | |
700 | 1 | |a Kim, Hyun-Cheol |4 oth | |
700 | 1 | |a Jang, Chan Joo |4 oth | |
700 | 1 | |a Kim, Yong Sun |4 oth | |
700 | 1 | |a Park, Jae-Hun |4 oth | |
773 | 0 | 8 | |i Enthalten in |n Elsevier |a Kamruzzaman, Md. ELSEVIER |t Investigating the urban heat island effect of transit oriented development in Brisbane |d 2017 |g New York, NY [u.a.] |w (DE-627)ELV000581879 |
773 | 1 | 8 | |g volume:195 |g year:2019 |g pages:30-37 |g extent:8 |
856 | 4 | 0 | |u https://doi.org/10.1016/j.jmarsys.2019.03.005 |3 Volltext |
912 | |a GBV_USEFLAG_U | ||
912 | |a GBV_ELV | ||
912 | |a SYSFLAG_U | ||
912 | |a SSG-OPC-GGO | ||
936 | b | k | |a 55.80 |j Verkehrswesen |j Transportwesen: Allgemeines |q VZ |
936 | b | k | |a 74.08 |j Wirtschaftsgeographie |q VZ |
936 | b | k | |a 74.75 |j Verkehrsplanung |j Verkehrspolitik |q VZ |
951 | |a AR | ||
952 | |d 195 |j 2019 |h 30-37 |g 8 |
author_variant |
d h dh |
---|---|
matchkey_str |
hahmdoshikrheetaesiekkimhyuncheoljangcha:2019----:nbevtoopiayrdcinnacdyosauwlignh |
hierarchy_sort_str |
2019transfer abstract |
bklnumber |
55.80 74.08 74.75 |
publishDate |
2019 |
allfields |
10.1016/j.jmarsys.2019.03.005 doi GBV00000000000613.pica (DE-627)ELV046518304 (ELSEVIER)S0924-7963(18)30279-3 DE-627 ger DE-627 rakwb eng 380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl Hahm, Doshik verfasserin aut An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea 2019transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. Rhee, Tae Siek oth Kim, Hyun-Cheol oth Jang, Chan Joo oth Kim, Yong Sun oth Park, Jae-Hun oth Enthalten in Elsevier Kamruzzaman, Md. ELSEVIER Investigating the urban heat island effect of transit oriented development in Brisbane 2017 New York, NY [u.a.] (DE-627)ELV000581879 volume:195 year:2019 pages:30-37 extent:8 https://doi.org/10.1016/j.jmarsys.2019.03.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO 55.80 Verkehrswesen Transportwesen: Allgemeines VZ 74.08 Wirtschaftsgeographie VZ 74.75 Verkehrsplanung Verkehrspolitik VZ AR 195 2019 30-37 8 |
spelling |
10.1016/j.jmarsys.2019.03.005 doi GBV00000000000613.pica (DE-627)ELV046518304 (ELSEVIER)S0924-7963(18)30279-3 DE-627 ger DE-627 rakwb eng 380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl Hahm, Doshik verfasserin aut An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea 2019transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. Rhee, Tae Siek oth Kim, Hyun-Cheol oth Jang, Chan Joo oth Kim, Yong Sun oth Park, Jae-Hun oth Enthalten in Elsevier Kamruzzaman, Md. ELSEVIER Investigating the urban heat island effect of transit oriented development in Brisbane 2017 New York, NY [u.a.] (DE-627)ELV000581879 volume:195 year:2019 pages:30-37 extent:8 https://doi.org/10.1016/j.jmarsys.2019.03.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO 55.80 Verkehrswesen Transportwesen: Allgemeines VZ 74.08 Wirtschaftsgeographie VZ 74.75 Verkehrsplanung Verkehrspolitik VZ AR 195 2019 30-37 8 |
allfields_unstemmed |
10.1016/j.jmarsys.2019.03.005 doi GBV00000000000613.pica (DE-627)ELV046518304 (ELSEVIER)S0924-7963(18)30279-3 DE-627 ger DE-627 rakwb eng 380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl Hahm, Doshik verfasserin aut An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea 2019transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. Rhee, Tae Siek oth Kim, Hyun-Cheol oth Jang, Chan Joo oth Kim, Yong Sun oth Park, Jae-Hun oth Enthalten in Elsevier Kamruzzaman, Md. ELSEVIER Investigating the urban heat island effect of transit oriented development in Brisbane 2017 New York, NY [u.a.] (DE-627)ELV000581879 volume:195 year:2019 pages:30-37 extent:8 https://doi.org/10.1016/j.jmarsys.2019.03.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO 55.80 Verkehrswesen Transportwesen: Allgemeines VZ 74.08 Wirtschaftsgeographie VZ 74.75 Verkehrsplanung Verkehrspolitik VZ AR 195 2019 30-37 8 |
allfieldsGer |
10.1016/j.jmarsys.2019.03.005 doi GBV00000000000613.pica (DE-627)ELV046518304 (ELSEVIER)S0924-7963(18)30279-3 DE-627 ger DE-627 rakwb eng 380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl Hahm, Doshik verfasserin aut An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea 2019transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. Rhee, Tae Siek oth Kim, Hyun-Cheol oth Jang, Chan Joo oth Kim, Yong Sun oth Park, Jae-Hun oth Enthalten in Elsevier Kamruzzaman, Md. ELSEVIER Investigating the urban heat island effect of transit oriented development in Brisbane 2017 New York, NY [u.a.] (DE-627)ELV000581879 volume:195 year:2019 pages:30-37 extent:8 https://doi.org/10.1016/j.jmarsys.2019.03.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO 55.80 Verkehrswesen Transportwesen: Allgemeines VZ 74.08 Wirtschaftsgeographie VZ 74.75 Verkehrsplanung Verkehrspolitik VZ AR 195 2019 30-37 8 |
allfieldsSound |
10.1016/j.jmarsys.2019.03.005 doi GBV00000000000613.pica (DE-627)ELV046518304 (ELSEVIER)S0924-7963(18)30279-3 DE-627 ger DE-627 rakwb eng 380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl Hahm, Doshik verfasserin aut An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea 2019transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. Rhee, Tae Siek oth Kim, Hyun-Cheol oth Jang, Chan Joo oth Kim, Yong Sun oth Park, Jae-Hun oth Enthalten in Elsevier Kamruzzaman, Md. ELSEVIER Investigating the urban heat island effect of transit oriented development in Brisbane 2017 New York, NY [u.a.] (DE-627)ELV000581879 volume:195 year:2019 pages:30-37 extent:8 https://doi.org/10.1016/j.jmarsys.2019.03.005 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO 55.80 Verkehrswesen Transportwesen: Allgemeines VZ 74.08 Wirtschaftsgeographie VZ 74.75 Verkehrsplanung Verkehrspolitik VZ AR 195 2019 30-37 8 |
language |
English |
source |
Enthalten in Investigating the urban heat island effect of transit oriented development in Brisbane New York, NY [u.a.] volume:195 year:2019 pages:30-37 extent:8 |
sourceStr |
Enthalten in Investigating the urban heat island effect of transit oriented development in Brisbane New York, NY [u.a.] volume:195 year:2019 pages:30-37 extent:8 |
format_phy_str_mv |
Article |
bklname |
Verkehrswesen Transportwesen: Allgemeines Wirtschaftsgeographie Verkehrsplanung Verkehrspolitik |
institution |
findex.gbv.de |
dewey-raw |
380 |
isfreeaccess_bool |
false |
container_title |
Investigating the urban heat island effect of transit oriented development in Brisbane |
authorswithroles_txt_mv |
Hahm, Doshik @@aut@@ Rhee, Tae Siek @@oth@@ Kim, Hyun-Cheol @@oth@@ Jang, Chan Joo @@oth@@ Kim, Yong Sun @@oth@@ Park, Jae-Hun @@oth@@ |
publishDateDaySort_date |
2019-01-01T00:00:00Z |
hierarchy_top_id |
ELV000581879 |
dewey-sort |
3380 |
id |
ELV046518304 |
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">ELV046518304</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626013837.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">191021s2019 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.jmarsys.2019.03.005</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBV00000000000613.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV046518304</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0924-7963(18)30279-3</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">380</subfield><subfield code="a">910</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">55.80</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">74.08</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">74.75</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Hahm, Doshik</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2019transfer abstract</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">8</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Rhee, Tae Siek</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kim, Hyun-Cheol</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jang, Chan Joo</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kim, Yong Sun</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Park, Jae-Hun</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier</subfield><subfield code="a">Kamruzzaman, Md. ELSEVIER</subfield><subfield code="t">Investigating the urban heat island effect of transit oriented development in Brisbane</subfield><subfield code="d">2017</subfield><subfield code="g">New York, NY [u.a.]</subfield><subfield code="w">(DE-627)ELV000581879</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:195</subfield><subfield code="g">year:2019</subfield><subfield code="g">pages:30-37</subfield><subfield code="g">extent:8</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.jmarsys.2019.03.005</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">55.80</subfield><subfield code="j">Verkehrswesen</subfield><subfield code="j">Transportwesen: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">74.08</subfield><subfield code="j">Wirtschaftsgeographie</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">74.75</subfield><subfield code="j">Verkehrsplanung</subfield><subfield code="j">Verkehrspolitik</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">195</subfield><subfield code="j">2019</subfield><subfield code="h">30-37</subfield><subfield code="g">8</subfield></datafield></record></collection>
|
author |
Hahm, Doshik |
spellingShingle |
Hahm, Doshik ddc 380 bkl 55.80 bkl 74.08 bkl 74.75 An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea |
authorStr |
Hahm, Doshik |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)ELV000581879 |
format |
electronic Article |
dewey-ones |
380 - Commerce, communications & transportation 910 - Geography & travel |
delete_txt_mv |
keep |
author_role |
aut |
collection |
elsevier |
remote_str |
true |
illustrated |
Not Illustrated |
topic_title |
380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea |
topic |
ddc 380 bkl 55.80 bkl 74.08 bkl 74.75 |
topic_unstemmed |
ddc 380 bkl 55.80 bkl 74.08 bkl 74.75 |
topic_browse |
ddc 380 bkl 55.80 bkl 74.08 bkl 74.75 |
format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
zu |
author2_variant |
t s r ts tsr h c k hck c j j cj cjj y s k ys ysk j h p jhp |
hierarchy_parent_title |
Investigating the urban heat island effect of transit oriented development in Brisbane |
hierarchy_parent_id |
ELV000581879 |
dewey-tens |
380 - Commerce, communications & transportation 910 - Geography & travel |
hierarchy_top_title |
Investigating the urban heat island effect of transit oriented development in Brisbane |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)ELV000581879 |
title |
An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea |
ctrlnum |
(DE-627)ELV046518304 (ELSEVIER)S0924-7963(18)30279-3 |
title_full |
An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea |
author_sort |
Hahm, Doshik |
journal |
Investigating the urban heat island effect of transit oriented development in Brisbane |
journalStr |
Investigating the urban heat island effect of transit oriented development in Brisbane |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
300 - Social sciences 900 - History & geography |
recordtype |
marc |
publishDateSort |
2019 |
contenttype_str_mv |
zzz |
container_start_page |
30 |
author_browse |
Hahm, Doshik |
container_volume |
195 |
physical |
8 |
class |
380 910 VZ 55.80 bkl 74.08 bkl 74.75 bkl |
format_se |
Elektronische Aufsätze |
author-letter |
Hahm, Doshik |
doi_str_mv |
10.1016/j.jmarsys.2019.03.005 |
dewey-full |
380 910 |
title_sort |
an observation of primary production enhanced by coastal upwelling in the southwest east/japan sea |
title_auth |
An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea |
abstract |
Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. |
abstractGer |
Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. |
abstract_unstemmed |
Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events. |
collection_details |
GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO |
title_short |
An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea |
url |
https://doi.org/10.1016/j.jmarsys.2019.03.005 |
remote_bool |
true |
author2 |
Rhee, Tae Siek Kim, Hyun-Cheol Jang, Chan Joo Kim, Yong Sun Park, Jae-Hun |
author2Str |
Rhee, Tae Siek Kim, Hyun-Cheol Jang, Chan Joo Kim, Yong Sun Park, Jae-Hun |
ppnlink |
ELV000581879 |
mediatype_str_mv |
z |
isOA_txt |
false |
hochschulschrift_bool |
false |
author2_role |
oth oth oth oth oth |
doi_str |
10.1016/j.jmarsys.2019.03.005 |
up_date |
2024-07-06T20:26:26.169Z |
_version_ |
1803862761715793920 |
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">ELV046518304</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626013837.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">191021s2019 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.jmarsys.2019.03.005</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBV00000000000613.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV046518304</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0924-7963(18)30279-3</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">380</subfield><subfield code="a">910</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">55.80</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">74.08</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">74.75</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Hahm, Doshik</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">An observation of primary production enhanced by coastal upwelling in the southwest East/Japan Sea</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2019transfer abstract</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">8</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Coastal upwelling (CU) is an important process that causes changes in physical and chemical properties, resulting in variation of biological processes in a coastal area. In the southwestern part of the East/Japan Sea (SWES), CU has been alleged as one of the mechanisms responsible for higher net primary production (NPP) than the rest of the East/Japan Sea. We provide, for the first time, high spatial resolution underway observations of sea surface temperature, salinity, chlorophyll-a fluorescence and Δ(O2/Ar), revealing the physical and biological characteristics of the upwelled waters in the SWES. The cold, upwelled waters retained high fluorescence and Δ(O2/Ar), consistent with enhanced phytoplankton biomass and biological O2 production by CU. The net community production (NCP) in the ambient and upwelled waters were 33 ± 19 and 77 ± 41 mmol O2 m−2 d−1, respectively. The latter should be considered as a lower bound, containing a significant fraction of low O2 waters from subsurface. Satellite observation indicated that NPP in the upwelled waters were higher than the ambient waters by 51%. This implies that up to half of higher NPP in the SWES than the rest of the East/Japan Sea can be ascribed to CU events.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Rhee, Tae Siek</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kim, Hyun-Cheol</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jang, Chan Joo</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kim, Yong Sun</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Park, Jae-Hun</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier</subfield><subfield code="a">Kamruzzaman, Md. ELSEVIER</subfield><subfield code="t">Investigating the urban heat island effect of transit oriented development in Brisbane</subfield><subfield code="d">2017</subfield><subfield code="g">New York, NY [u.a.]</subfield><subfield code="w">(DE-627)ELV000581879</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:195</subfield><subfield code="g">year:2019</subfield><subfield code="g">pages:30-37</subfield><subfield code="g">extent:8</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.jmarsys.2019.03.005</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">55.80</subfield><subfield code="j">Verkehrswesen</subfield><subfield code="j">Transportwesen: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">74.08</subfield><subfield code="j">Wirtschaftsgeographie</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">74.75</subfield><subfield code="j">Verkehrsplanung</subfield><subfield code="j">Verkehrspolitik</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">195</subfield><subfield code="j">2019</subfield><subfield code="h">30-37</subfield><subfield code="g">8</subfield></datafield></record></collection>
|
score |
7.399686 |