Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model
Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Yoshi N Sasaki [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2017 |
|---|
| Schlagwörter: |
|---|
| Systematik: |
|
|---|
| Übergeordnetes Werk: |
Enthalten in: Journal of climate - Boston, Mass. [u.a.] : AMS, 1988, 30(2017), 14, Seite 5585 |
|---|---|
| Übergeordnetes Werk: |
volume:30 ; year:2017 ; number:14 ; pages:5585 |
| Links: |
|---|
| Katalog-ID: |
OLC1996223046 |
|---|
| LEADER | 01000caa a2200265 4500 | ||
|---|---|---|---|
| 001 | OLC1996223046 | ||
| 003 | DE-627 | ||
| 005 | 20220221061900.0 | ||
| 007 | tu | ||
| 008 | 170901s2017 xx ||||| 00| ||eng c | ||
| 028 | 5 | 2 | |a PQ20171125 |
| 035 | |a (DE-627)OLC1996223046 | ||
| 035 | |a (DE-599)GBVOLC1996223046 | ||
| 035 | |a (PRQ)p934-d17efc7c16098ba5557a8987e87c34669c740edc4255e60131d4cf813aeee260 | ||
| 035 | |a (KEY)0166131020170000030001405585sealevelvariabilityaroundjapanduringthetwentiethce | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |q DE-600 |
| 084 | |a UA 4548 |q AVZ |2 rvk | ||
| 084 | |a 38.82 |2 bkl | ||
| 100 | 0 | |a Yoshi N Sasaki |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model |
| 264 | 1 | |c 2017 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 520 | |a Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales. | ||
| 650 | 4 | |a Wind stress | |
| 650 | 4 | |a Variability | |
| 650 | 4 | |a Sea level | |
| 650 | 4 | |a Coastal environments | |
| 650 | 4 | |a Time series | |
| 650 | 4 | |a Sea level rise | |
| 650 | 4 | |a High seas | |
| 650 | 4 | |a Fresh water | |
| 650 | 4 | |a Computer simulation | |
| 650 | 4 | |a Wind effects | |
| 650 | 4 | |a Aleutian low | |
| 650 | 4 | |a Wind | |
| 650 | 4 | |a Coasts | |
| 650 | 4 | |a Web sites | |
| 650 | 4 | |a Level (quantity) | |
| 650 | 4 | |a Climate models | |
| 650 | 4 | |a Natural variability | |
| 650 | 4 | |a Studies | |
| 650 | 4 | |a Inland water environment | |
| 650 | 4 | |a 20th century | |
| 650 | 4 | |a Trends | |
| 650 | 4 | |a Curl (vectors) | |
| 650 | 4 | |a Sea level variability | |
| 650 | 4 | |a Oceanic analysis | |
| 650 | 4 | |a Wind stress curl | |
| 650 | 4 | |a Sea level changes | |
| 700 | 0 | |a Ryosuke Washizu |4 oth | |
| 700 | 0 | |a Tamaki Yasuda |4 oth | |
| 700 | 0 | |a Shoshiro Minobe |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |t Journal of climate |d Boston, Mass. [u.a.] : AMS, 1988 |g 30(2017), 14, Seite 5585 |w (DE-627)129622311 |w (DE-600)246750-1 |w (DE-576)018141331 |x 0894-8755 |7 nnns |
| 773 | 1 | 8 | |g volume:30 |g year:2017 |g number:14 |g pages:5585 |
| 856 | 4 | 2 | |u https://search.proquest.com/docview/1924770358 |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OLC-FOR | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a GBV_ILN_62 | ||
| 912 | |a GBV_ILN_154 | ||
| 912 | |a GBV_ILN_601 | ||
| 912 | |a GBV_ILN_2010 | ||
| 912 | |a GBV_ILN_2012 | ||
| 936 | r | v | |a UA 4548 |
| 936 | b | k | |a 38.82 |q AVZ |
| 951 | |a AR | ||
| 952 | |d 30 |j 2017 |e 14 |h 5585 | ||
| author_variant |
y n s yns |
|---|---|
| matchkey_str |
article:08948755:2017----::elvlaibltaonjpnuightetehetrsmlt |
| hierarchy_sort_str |
2017 |
| bklnumber |
38.82 |
| publishDate |
2017 |
| allfields |
PQ20171125 (DE-627)OLC1996223046 (DE-599)GBVOLC1996223046 (PRQ)p934-d17efc7c16098ba5557a8987e87c34669c740edc4255e60131d4cf813aeee260 (KEY)0166131020170000030001405585sealevelvariabilityaroundjapanduringthetwentiethce DE-627 ger DE-627 rakwb eng 550 DE-600 UA 4548 AVZ rvk 38.82 bkl Yoshi N Sasaki verfasserin aut Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales. Wind stress Variability Sea level Coastal environments Time series Sea level rise High seas Fresh water Computer simulation Wind effects Aleutian low Wind Coasts Web sites Level (quantity) Climate models Natural variability Studies Inland water environment 20th century Trends Curl (vectors) Sea level variability Oceanic analysis Wind stress curl Sea level changes Ryosuke Washizu oth Tamaki Yasuda oth Shoshiro Minobe oth Enthalten in Journal of climate Boston, Mass. [u.a.] : AMS, 1988 30(2017), 14, Seite 5585 (DE-627)129622311 (DE-600)246750-1 (DE-576)018141331 0894-8755 nnns volume:30 year:2017 number:14 pages:5585 https://search.proquest.com/docview/1924770358 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2012 UA 4548 38.82 AVZ AR 30 2017 14 5585 |
| spelling |
PQ20171125 (DE-627)OLC1996223046 (DE-599)GBVOLC1996223046 (PRQ)p934-d17efc7c16098ba5557a8987e87c34669c740edc4255e60131d4cf813aeee260 (KEY)0166131020170000030001405585sealevelvariabilityaroundjapanduringthetwentiethce DE-627 ger DE-627 rakwb eng 550 DE-600 UA 4548 AVZ rvk 38.82 bkl Yoshi N Sasaki verfasserin aut Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales. Wind stress Variability Sea level Coastal environments Time series Sea level rise High seas Fresh water Computer simulation Wind effects Aleutian low Wind Coasts Web sites Level (quantity) Climate models Natural variability Studies Inland water environment 20th century Trends Curl (vectors) Sea level variability Oceanic analysis Wind stress curl Sea level changes Ryosuke Washizu oth Tamaki Yasuda oth Shoshiro Minobe oth Enthalten in Journal of climate Boston, Mass. [u.a.] : AMS, 1988 30(2017), 14, Seite 5585 (DE-627)129622311 (DE-600)246750-1 (DE-576)018141331 0894-8755 nnns volume:30 year:2017 number:14 pages:5585 https://search.proquest.com/docview/1924770358 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2012 UA 4548 38.82 AVZ AR 30 2017 14 5585 |
| allfields_unstemmed |
PQ20171125 (DE-627)OLC1996223046 (DE-599)GBVOLC1996223046 (PRQ)p934-d17efc7c16098ba5557a8987e87c34669c740edc4255e60131d4cf813aeee260 (KEY)0166131020170000030001405585sealevelvariabilityaroundjapanduringthetwentiethce DE-627 ger DE-627 rakwb eng 550 DE-600 UA 4548 AVZ rvk 38.82 bkl Yoshi N Sasaki verfasserin aut Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales. Wind stress Variability Sea level Coastal environments Time series Sea level rise High seas Fresh water Computer simulation Wind effects Aleutian low Wind Coasts Web sites Level (quantity) Climate models Natural variability Studies Inland water environment 20th century Trends Curl (vectors) Sea level variability Oceanic analysis Wind stress curl Sea level changes Ryosuke Washizu oth Tamaki Yasuda oth Shoshiro Minobe oth Enthalten in Journal of climate Boston, Mass. [u.a.] : AMS, 1988 30(2017), 14, Seite 5585 (DE-627)129622311 (DE-600)246750-1 (DE-576)018141331 0894-8755 nnns volume:30 year:2017 number:14 pages:5585 https://search.proquest.com/docview/1924770358 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2012 UA 4548 38.82 AVZ AR 30 2017 14 5585 |
| allfieldsGer |
PQ20171125 (DE-627)OLC1996223046 (DE-599)GBVOLC1996223046 (PRQ)p934-d17efc7c16098ba5557a8987e87c34669c740edc4255e60131d4cf813aeee260 (KEY)0166131020170000030001405585sealevelvariabilityaroundjapanduringthetwentiethce DE-627 ger DE-627 rakwb eng 550 DE-600 UA 4548 AVZ rvk 38.82 bkl Yoshi N Sasaki verfasserin aut Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales. Wind stress Variability Sea level Coastal environments Time series Sea level rise High seas Fresh water Computer simulation Wind effects Aleutian low Wind Coasts Web sites Level (quantity) Climate models Natural variability Studies Inland water environment 20th century Trends Curl (vectors) Sea level variability Oceanic analysis Wind stress curl Sea level changes Ryosuke Washizu oth Tamaki Yasuda oth Shoshiro Minobe oth Enthalten in Journal of climate Boston, Mass. [u.a.] : AMS, 1988 30(2017), 14, Seite 5585 (DE-627)129622311 (DE-600)246750-1 (DE-576)018141331 0894-8755 nnns volume:30 year:2017 number:14 pages:5585 https://search.proquest.com/docview/1924770358 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2012 UA 4548 38.82 AVZ AR 30 2017 14 5585 |
| allfieldsSound |
PQ20171125 (DE-627)OLC1996223046 (DE-599)GBVOLC1996223046 (PRQ)p934-d17efc7c16098ba5557a8987e87c34669c740edc4255e60131d4cf813aeee260 (KEY)0166131020170000030001405585sealevelvariabilityaroundjapanduringthetwentiethce DE-627 ger DE-627 rakwb eng 550 DE-600 UA 4548 AVZ rvk 38.82 bkl Yoshi N Sasaki verfasserin aut Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales. Wind stress Variability Sea level Coastal environments Time series Sea level rise High seas Fresh water Computer simulation Wind effects Aleutian low Wind Coasts Web sites Level (quantity) Climate models Natural variability Studies Inland water environment 20th century Trends Curl (vectors) Sea level variability Oceanic analysis Wind stress curl Sea level changes Ryosuke Washizu oth Tamaki Yasuda oth Shoshiro Minobe oth Enthalten in Journal of climate Boston, Mass. [u.a.] : AMS, 1988 30(2017), 14, Seite 5585 (DE-627)129622311 (DE-600)246750-1 (DE-576)018141331 0894-8755 nnns volume:30 year:2017 number:14 pages:5585 https://search.proquest.com/docview/1924770358 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2012 UA 4548 38.82 AVZ AR 30 2017 14 5585 |
| language |
English |
| source |
Enthalten in Journal of climate 30(2017), 14, Seite 5585 volume:30 year:2017 number:14 pages:5585 |
| sourceStr |
Enthalten in Journal of climate 30(2017), 14, Seite 5585 volume:30 year:2017 number:14 pages:5585 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Wind stress Variability Sea level Coastal environments Time series Sea level rise High seas Fresh water Computer simulation Wind effects Aleutian low Wind Coasts Web sites Level (quantity) Climate models Natural variability Studies Inland water environment 20th century Trends Curl (vectors) Sea level variability Oceanic analysis Wind stress curl Sea level changes |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Journal of climate |
| authorswithroles_txt_mv |
Yoshi N Sasaki @@aut@@ Ryosuke Washizu @@oth@@ Tamaki Yasuda @@oth@@ Shoshiro Minobe @@oth@@ |
| publishDateDaySort_date |
2017-01-01T00:00:00Z |
| hierarchy_top_id |
129622311 |
| dewey-sort |
3550 |
| id |
OLC1996223046 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1996223046</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220221061900.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">170901s2017 xx ||||| 00| ||eng c</controlfield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20171125</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1996223046</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1996223046</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p934-d17efc7c16098ba5557a8987e87c34669c740edc4255e60131d4cf813aeee260</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0166131020170000030001405585sealevelvariabilityaroundjapanduringthetwentiethce</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">UA 4548</subfield><subfield code="q">AVZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.82</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Yoshi N Sasaki</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</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">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Wind stress</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Variability</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Coastal environments</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Time series</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level rise</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">High seas</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Fresh water</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Computer simulation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Wind effects</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Aleutian low</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Wind</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Coasts</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Web sites</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Level (quantity)</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Climate models</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Natural variability</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Studies</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Inland water environment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">20th century</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Trends</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Curl (vectors)</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level variability</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Oceanic analysis</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Wind stress curl</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level changes</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Ryosuke Washizu</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Tamaki Yasuda</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Shoshiro Minobe</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of climate</subfield><subfield code="d">Boston, Mass. [u.a.] : AMS, 1988</subfield><subfield code="g">30(2017), 14, Seite 5585</subfield><subfield code="w">(DE-627)129622311</subfield><subfield code="w">(DE-600)246750-1</subfield><subfield code="w">(DE-576)018141331</subfield><subfield code="x">0894-8755</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:30</subfield><subfield code="g">year:2017</subfield><subfield code="g">number:14</subfield><subfield code="g">pages:5585</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://search.proquest.com/docview/1924770358</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_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</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_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2012</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">UA 4548</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.82</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">30</subfield><subfield code="j">2017</subfield><subfield code="e">14</subfield><subfield code="h">5585</subfield></datafield></record></collection>
|
| author |
Yoshi N Sasaki |
| spellingShingle |
Yoshi N Sasaki ddc 550 rvk UA 4548 bkl 38.82 misc Wind stress misc Variability misc Sea level misc Coastal environments misc Time series misc Sea level rise misc High seas misc Fresh water misc Computer simulation misc Wind effects misc Aleutian low misc Wind misc Coasts misc Web sites misc Level (quantity) misc Climate models misc Natural variability misc Studies misc Inland water environment misc 20th century misc Trends misc Curl (vectors) misc Sea level variability misc Oceanic analysis misc Wind stress curl misc Sea level changes Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model |
| authorStr |
Yoshi N Sasaki |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)129622311 |
| format |
Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0894-8755 |
| topic_title |
550 DE-600 UA 4548 AVZ rvk 38.82 bkl Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model Wind stress Variability Sea level Coastal environments Time series Sea level rise High seas Fresh water Computer simulation Wind effects Aleutian low Wind Coasts Web sites Level (quantity) Climate models Natural variability Studies Inland water environment 20th century Trends Curl (vectors) Sea level variability Oceanic analysis Wind stress curl Sea level changes |
| topic |
ddc 550 rvk UA 4548 bkl 38.82 misc Wind stress misc Variability misc Sea level misc Coastal environments misc Time series misc Sea level rise misc High seas misc Fresh water misc Computer simulation misc Wind effects misc Aleutian low misc Wind misc Coasts misc Web sites misc Level (quantity) misc Climate models misc Natural variability misc Studies misc Inland water environment misc 20th century misc Trends misc Curl (vectors) misc Sea level variability misc Oceanic analysis misc Wind stress curl misc Sea level changes |
| topic_unstemmed |
ddc 550 rvk UA 4548 bkl 38.82 misc Wind stress misc Variability misc Sea level misc Coastal environments misc Time series misc Sea level rise misc High seas misc Fresh water misc Computer simulation misc Wind effects misc Aleutian low misc Wind misc Coasts misc Web sites misc Level (quantity) misc Climate models misc Natural variability misc Studies misc Inland water environment misc 20th century misc Trends misc Curl (vectors) misc Sea level variability misc Oceanic analysis misc Wind stress curl misc Sea level changes |
| topic_browse |
ddc 550 rvk UA 4548 bkl 38.82 misc Wind stress misc Variability misc Sea level misc Coastal environments misc Time series misc Sea level rise misc High seas misc Fresh water misc Computer simulation misc Wind effects misc Aleutian low misc Wind misc Coasts misc Web sites misc Level (quantity) misc Climate models misc Natural variability misc Studies misc Inland water environment misc 20th century misc Trends misc Curl (vectors) misc Sea level variability misc Oceanic analysis misc Wind stress curl misc Sea level changes |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| author2_variant |
r w rw t y ty s m sm |
| hierarchy_parent_title |
Journal of climate |
| hierarchy_parent_id |
129622311 |
| dewey-tens |
550 - Earth sciences & geology |
| hierarchy_top_title |
Journal of climate |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)129622311 (DE-600)246750-1 (DE-576)018141331 |
| title |
Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model |
| ctrlnum |
(DE-627)OLC1996223046 (DE-599)GBVOLC1996223046 (PRQ)p934-d17efc7c16098ba5557a8987e87c34669c740edc4255e60131d4cf813aeee260 (KEY)0166131020170000030001405585sealevelvariabilityaroundjapanduringthetwentiethce |
| title_full |
Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model |
| author_sort |
Yoshi N Sasaki |
| journal |
Journal of climate |
| journalStr |
Journal of climate |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2017 |
| contenttype_str_mv |
txt |
| container_start_page |
5585 |
| author_browse |
Yoshi N Sasaki |
| container_volume |
30 |
| class |
550 DE-600 UA 4548 AVZ rvk 38.82 bkl |
| format_se |
Aufsätze |
| author-letter |
Yoshi N Sasaki |
| dewey-full |
550 |
| title_sort |
sea level variability around japan during the twentieth century simulated by a regional ocean model |
| title_auth |
Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model |
| abstract |
Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales. |
| abstractGer |
Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales. |
| abstract_unstemmed |
Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales. |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2010 GBV_ILN_2012 |
| container_issue |
14 |
| title_short |
Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model |
| url |
https://search.proquest.com/docview/1924770358 |
| remote_bool |
false |
| author2 |
Ryosuke Washizu Tamaki Yasuda Shoshiro Minobe |
| author2Str |
Ryosuke Washizu Tamaki Yasuda Shoshiro Minobe |
| ppnlink |
129622311 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth |
| up_date |
2024-07-04T00:12:42.966Z |
| _version_ |
1803605207121133568 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1996223046</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220221061900.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">170901s2017 xx ||||| 00| ||eng c</controlfield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20171125</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1996223046</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1996223046</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p934-d17efc7c16098ba5557a8987e87c34669c740edc4255e60131d4cf813aeee260</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0166131020170000030001405585sealevelvariabilityaroundjapanduringthetwentiethce</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">UA 4548</subfield><subfield code="q">AVZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.82</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Yoshi N Sasaki</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Sea Level Variability around Japan during the Twentieth Century Simulated by a Regional Ocean Model</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</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">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Sea level variability around Japan from 1906 to 2010 is examined using a regional ocean model, along with observational data and the CMIP5 historical simulations. The regional model reproduces observed interdecadal sea level variability, for example, high sea level around 1950, low sea level in the 1970s, and sea level rise during the most recent three decades, along the Japanese coast. Sensitivity runs reveal that the high sea level around 1950 was induced by the wind stress curl changes over the North Pacific, characterized by a weakening of the Aleutian low. In contrast, the recent sea level rise is primarily caused by heat and freshwater flux forcings. That the wind-induced sea level rise along the Japanese coast around 1950 is as large as the recent sea level rise highlights the importance of natural variability in understanding regional sea level change on interdecadal time scales.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Wind stress</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Variability</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Coastal environments</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Time series</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level rise</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">High seas</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Fresh water</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Computer simulation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Wind effects</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Aleutian low</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Wind</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Coasts</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Web sites</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Level (quantity)</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Climate models</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Natural variability</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Studies</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Inland water environment</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">20th century</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Trends</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Curl (vectors)</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level variability</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Oceanic analysis</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Wind stress curl</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level changes</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Ryosuke Washizu</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Tamaki Yasuda</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Shoshiro Minobe</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of climate</subfield><subfield code="d">Boston, Mass. [u.a.] : AMS, 1988</subfield><subfield code="g">30(2017), 14, Seite 5585</subfield><subfield code="w">(DE-627)129622311</subfield><subfield code="w">(DE-600)246750-1</subfield><subfield code="w">(DE-576)018141331</subfield><subfield code="x">0894-8755</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:30</subfield><subfield code="g">year:2017</subfield><subfield code="g">number:14</subfield><subfield code="g">pages:5585</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://search.proquest.com/docview/1924770358</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_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</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_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2012</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">UA 4548</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.82</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">30</subfield><subfield code="j">2017</subfield><subfield code="e">14</subfield><subfield code="h">5585</subfield></datafield></record></collection>
|
| score |
7.4013977 |