Hydrological drivers of record‐setting water level rise on Earth's largest lake system
Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided w...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Gronewold, A. D [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2016 |
|---|
| Rechteinformationen: |
Nutzungsrecht: © 2016. American Geophysical Union. All Rights Reserved. |
|---|
| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: Water resources research - Hoboken, NJ : Wiley, 1965, 52(2016), 5, Seite 4026-4042 |
|---|---|
| Übergeordnetes Werk: |
volume:52 ; year:2016 ; number:5 ; pages:4026-4042 |
| Links: |
|---|
| DOI / URN: |
10.1002/2015WR018209 |
|---|
| Katalog-ID: |
OLC1977463010 |
|---|
| LEADER | 01000caa a2200265 4500 | ||
|---|---|---|---|
| 001 | OLC1977463010 | ||
| 003 | DE-627 | ||
| 005 | 20220221191544.0 | ||
| 007 | tu | ||
| 008 | 160719s2016 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1002/2015WR018209 |2 doi | |
| 028 | 5 | 2 | |a PQ20160719 |
| 035 | |a (DE-627)OLC1977463010 | ||
| 035 | |a (DE-599)GBVOLC1977463010 | ||
| 035 | |a (PRQ)p962-5a5166a5bd9e657206aa489a74f9228d83dd52cafafecae3b3eafd61fabc7ddf0 | ||
| 035 | |a (KEY)0046260820160000052000504026hydrologicaldriversofrecordsettingwaterlevelriseon | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |q DNB |
| 084 | |a 38.85 |2 bkl | ||
| 100 | 1 | |a Gronewold, A. D |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Hydrological drivers of record‐setting water level rise on Earth's largest lake system |
| 264 | 1 | |c 2016 | |
| 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 Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels | ||
| 540 | |a Nutzungsrecht: © 2016. American Geophysical Union. All Rights Reserved. | ||
| 650 | 4 | |a Bayesian | |
| 650 | 4 | |a Great Lakes | |
| 650 | 4 | |a water balance | |
| 650 | 4 | |a hydrological cycle | |
| 650 | 4 | |a Hydrology | |
| 650 | 4 | |a Lakes | |
| 650 | 4 | |a Precipitation | |
| 650 | 4 | |a Sea level | |
| 650 | 4 | |a Earth | |
| 650 | 4 | |a Runoff | |
| 700 | 1 | |a Bruxer, J |4 oth | |
| 700 | 1 | |a Durnford, D |4 oth | |
| 700 | 1 | |a Smith, J. P |4 oth | |
| 700 | 1 | |a Clites, A. H |4 oth | |
| 700 | 1 | |a Seglenieks, F |4 oth | |
| 700 | 1 | |a Qian, S. S |4 oth | |
| 700 | 1 | |a Hunter, T. S |4 oth | |
| 700 | 1 | |a Fortin, V |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |t Water resources research |d Hoboken, NJ : Wiley, 1965 |g 52(2016), 5, Seite 4026-4042 |w (DE-627)129088285 |w (DE-600)5564-5 |w (DE-576)014422980 |x 0043-1397 |7 nnns |
| 773 | 1 | 8 | |g volume:52 |g year:2016 |g number:5 |g pages:4026-4042 |
| 856 | 4 | 1 | |u http://dx.doi.org/10.1002/2015WR018209 |3 Volltext |
| 856 | 4 | 2 | |u http://onlinelibrary.wiley.com/doi/10.1002/2015WR018209/abstract |
| 856 | 4 | 2 | |u http://search.proquest.com/docview/1798180315 |
| 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_4219 | ||
| 936 | b | k | |a 38.85 |q AVZ |
| 951 | |a AR | ||
| 952 | |d 52 |j 2016 |e 5 |h 4026-4042 | ||
| author_variant |
a d g ad adg |
|---|---|
| matchkey_str |
article:00431397:2016----::yrlgclrvrorcrstigaelvlienat |
| hierarchy_sort_str |
2016 |
| bklnumber |
38.85 |
| publishDate |
2016 |
| allfields |
10.1002/2015WR018209 doi PQ20160719 (DE-627)OLC1977463010 (DE-599)GBVOLC1977463010 (PRQ)p962-5a5166a5bd9e657206aa489a74f9228d83dd52cafafecae3b3eafd61fabc7ddf0 (KEY)0046260820160000052000504026hydrologicaldriversofrecordsettingwaterlevelriseon DE-627 ger DE-627 rakwb eng 550 DNB 38.85 bkl Gronewold, A. D verfasserin aut Hydrological drivers of record‐setting water level rise on Earth's largest lake system 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels Nutzungsrecht: © 2016. American Geophysical Union. All Rights Reserved. Bayesian Great Lakes water balance hydrological cycle Hydrology Lakes Precipitation Sea level Earth Runoff Bruxer, J oth Durnford, D oth Smith, J. P oth Clites, A. H oth Seglenieks, F oth Qian, S. S oth Hunter, T. S oth Fortin, V oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 52(2016), 5, Seite 4026-4042 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:52 year:2016 number:5 pages:4026-4042 http://dx.doi.org/10.1002/2015WR018209 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015WR018209/abstract http://search.proquest.com/docview/1798180315 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_4219 38.85 AVZ AR 52 2016 5 4026-4042 |
| spelling |
10.1002/2015WR018209 doi PQ20160719 (DE-627)OLC1977463010 (DE-599)GBVOLC1977463010 (PRQ)p962-5a5166a5bd9e657206aa489a74f9228d83dd52cafafecae3b3eafd61fabc7ddf0 (KEY)0046260820160000052000504026hydrologicaldriversofrecordsettingwaterlevelriseon DE-627 ger DE-627 rakwb eng 550 DNB 38.85 bkl Gronewold, A. D verfasserin aut Hydrological drivers of record‐setting water level rise on Earth's largest lake system 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels Nutzungsrecht: © 2016. American Geophysical Union. All Rights Reserved. Bayesian Great Lakes water balance hydrological cycle Hydrology Lakes Precipitation Sea level Earth Runoff Bruxer, J oth Durnford, D oth Smith, J. P oth Clites, A. H oth Seglenieks, F oth Qian, S. S oth Hunter, T. S oth Fortin, V oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 52(2016), 5, Seite 4026-4042 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:52 year:2016 number:5 pages:4026-4042 http://dx.doi.org/10.1002/2015WR018209 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015WR018209/abstract http://search.proquest.com/docview/1798180315 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_4219 38.85 AVZ AR 52 2016 5 4026-4042 |
| allfields_unstemmed |
10.1002/2015WR018209 doi PQ20160719 (DE-627)OLC1977463010 (DE-599)GBVOLC1977463010 (PRQ)p962-5a5166a5bd9e657206aa489a74f9228d83dd52cafafecae3b3eafd61fabc7ddf0 (KEY)0046260820160000052000504026hydrologicaldriversofrecordsettingwaterlevelriseon DE-627 ger DE-627 rakwb eng 550 DNB 38.85 bkl Gronewold, A. D verfasserin aut Hydrological drivers of record‐setting water level rise on Earth's largest lake system 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels Nutzungsrecht: © 2016. American Geophysical Union. All Rights Reserved. Bayesian Great Lakes water balance hydrological cycle Hydrology Lakes Precipitation Sea level Earth Runoff Bruxer, J oth Durnford, D oth Smith, J. P oth Clites, A. H oth Seglenieks, F oth Qian, S. S oth Hunter, T. S oth Fortin, V oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 52(2016), 5, Seite 4026-4042 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:52 year:2016 number:5 pages:4026-4042 http://dx.doi.org/10.1002/2015WR018209 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015WR018209/abstract http://search.proquest.com/docview/1798180315 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_4219 38.85 AVZ AR 52 2016 5 4026-4042 |
| allfieldsGer |
10.1002/2015WR018209 doi PQ20160719 (DE-627)OLC1977463010 (DE-599)GBVOLC1977463010 (PRQ)p962-5a5166a5bd9e657206aa489a74f9228d83dd52cafafecae3b3eafd61fabc7ddf0 (KEY)0046260820160000052000504026hydrologicaldriversofrecordsettingwaterlevelriseon DE-627 ger DE-627 rakwb eng 550 DNB 38.85 bkl Gronewold, A. D verfasserin aut Hydrological drivers of record‐setting water level rise on Earth's largest lake system 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels Nutzungsrecht: © 2016. American Geophysical Union. All Rights Reserved. Bayesian Great Lakes water balance hydrological cycle Hydrology Lakes Precipitation Sea level Earth Runoff Bruxer, J oth Durnford, D oth Smith, J. P oth Clites, A. H oth Seglenieks, F oth Qian, S. S oth Hunter, T. S oth Fortin, V oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 52(2016), 5, Seite 4026-4042 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:52 year:2016 number:5 pages:4026-4042 http://dx.doi.org/10.1002/2015WR018209 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015WR018209/abstract http://search.proquest.com/docview/1798180315 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_4219 38.85 AVZ AR 52 2016 5 4026-4042 |
| allfieldsSound |
10.1002/2015WR018209 doi PQ20160719 (DE-627)OLC1977463010 (DE-599)GBVOLC1977463010 (PRQ)p962-5a5166a5bd9e657206aa489a74f9228d83dd52cafafecae3b3eafd61fabc7ddf0 (KEY)0046260820160000052000504026hydrologicaldriversofrecordsettingwaterlevelriseon DE-627 ger DE-627 rakwb eng 550 DNB 38.85 bkl Gronewold, A. D verfasserin aut Hydrological drivers of record‐setting water level rise on Earth's largest lake system 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels Nutzungsrecht: © 2016. American Geophysical Union. All Rights Reserved. Bayesian Great Lakes water balance hydrological cycle Hydrology Lakes Precipitation Sea level Earth Runoff Bruxer, J oth Durnford, D oth Smith, J. P oth Clites, A. H oth Seglenieks, F oth Qian, S. S oth Hunter, T. S oth Fortin, V oth Enthalten in Water resources research Hoboken, NJ : Wiley, 1965 52(2016), 5, Seite 4026-4042 (DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 0043-1397 nnns volume:52 year:2016 number:5 pages:4026-4042 http://dx.doi.org/10.1002/2015WR018209 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015WR018209/abstract http://search.proquest.com/docview/1798180315 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_4219 38.85 AVZ AR 52 2016 5 4026-4042 |
| language |
English |
| source |
Enthalten in Water resources research 52(2016), 5, Seite 4026-4042 volume:52 year:2016 number:5 pages:4026-4042 |
| sourceStr |
Enthalten in Water resources research 52(2016), 5, Seite 4026-4042 volume:52 year:2016 number:5 pages:4026-4042 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Bayesian Great Lakes water balance hydrological cycle Hydrology Lakes Precipitation Sea level Earth Runoff |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Water resources research |
| authorswithroles_txt_mv |
Gronewold, A. D @@aut@@ Bruxer, J @@oth@@ Durnford, D @@oth@@ Smith, J. P @@oth@@ Clites, A. H @@oth@@ Seglenieks, F @@oth@@ Qian, S. S @@oth@@ Hunter, T. S @@oth@@ Fortin, V @@oth@@ |
| publishDateDaySort_date |
2016-01-01T00:00:00Z |
| hierarchy_top_id |
129088285 |
| dewey-sort |
3550 |
| id |
OLC1977463010 |
| 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">OLC1977463010</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220221191544.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">160719s2016 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1002/2015WR018209</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20160719</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1977463010</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1977463010</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p962-5a5166a5bd9e657206aa489a74f9228d83dd52cafafecae3b3eafd61fabc7ddf0</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0046260820160000052000504026hydrologicaldriversofrecordsettingwaterlevelriseon</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">DNB</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.85</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Gronewold, A. D</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Hydrological drivers of record‐setting water level rise on Earth's largest lake system</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</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">Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: © 2016. American Geophysical Union. All Rights Reserved.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Bayesian</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Great Lakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">water balance</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">hydrological cycle</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Hydrology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Lakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Precipitation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Runoff</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bruxer, J</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Durnford, D</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Smith, J. P</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Clites, A. H</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Seglenieks, F</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Qian, S. S</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Hunter, T. S</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fortin, V</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Water resources research</subfield><subfield code="d">Hoboken, NJ : Wiley, 1965</subfield><subfield code="g">52(2016), 5, Seite 4026-4042</subfield><subfield code="w">(DE-627)129088285</subfield><subfield code="w">(DE-600)5564-5</subfield><subfield code="w">(DE-576)014422980</subfield><subfield code="x">0043-1397</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:52</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:5</subfield><subfield code="g">pages:4026-4042</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1002/2015WR018209</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://onlinelibrary.wiley.com/doi/10.1002/2015WR018209/abstract</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1798180315</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_4219</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.85</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">52</subfield><subfield code="j">2016</subfield><subfield code="e">5</subfield><subfield code="h">4026-4042</subfield></datafield></record></collection>
|
| author |
Gronewold, A. D |
| spellingShingle |
Gronewold, A. D ddc 550 bkl 38.85 misc Bayesian misc Great Lakes misc water balance misc hydrological cycle misc Hydrology misc Lakes misc Precipitation misc Sea level misc Earth misc Runoff Hydrological drivers of record‐setting water level rise on Earth's largest lake system |
| authorStr |
Gronewold, A. D |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)129088285 |
| format |
Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0043-1397 |
| topic_title |
550 DNB 38.85 bkl Hydrological drivers of record‐setting water level rise on Earth's largest lake system Bayesian Great Lakes water balance hydrological cycle Hydrology Lakes Precipitation Sea level Earth Runoff |
| topic |
ddc 550 bkl 38.85 misc Bayesian misc Great Lakes misc water balance misc hydrological cycle misc Hydrology misc Lakes misc Precipitation misc Sea level misc Earth misc Runoff |
| topic_unstemmed |
ddc 550 bkl 38.85 misc Bayesian misc Great Lakes misc water balance misc hydrological cycle misc Hydrology misc Lakes misc Precipitation misc Sea level misc Earth misc Runoff |
| topic_browse |
ddc 550 bkl 38.85 misc Bayesian misc Great Lakes misc water balance misc hydrological cycle misc Hydrology misc Lakes misc Precipitation misc Sea level misc Earth misc Runoff |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| author2_variant |
j b jb d d dd j p s jp jps a h c ah ahc f s fs s s q ss ssq t s h ts tsh v f vf |
| hierarchy_parent_title |
Water resources research |
| hierarchy_parent_id |
129088285 |
| dewey-tens |
550 - Earth sciences & geology |
| hierarchy_top_title |
Water resources research |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)129088285 (DE-600)5564-5 (DE-576)014422980 |
| title |
Hydrological drivers of record‐setting water level rise on Earth's largest lake system |
| ctrlnum |
(DE-627)OLC1977463010 (DE-599)GBVOLC1977463010 (PRQ)p962-5a5166a5bd9e657206aa489a74f9228d83dd52cafafecae3b3eafd61fabc7ddf0 (KEY)0046260820160000052000504026hydrologicaldriversofrecordsettingwaterlevelriseon |
| title_full |
Hydrological drivers of record‐setting water level rise on Earth's largest lake system |
| author_sort |
Gronewold, A. D |
| journal |
Water resources research |
| journalStr |
Water resources research |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2016 |
| contenttype_str_mv |
txt |
| container_start_page |
4026 |
| author_browse |
Gronewold, A. D |
| container_volume |
52 |
| class |
550 DNB 38.85 bkl |
| format_se |
Aufsätze |
| author-letter |
Gronewold, A. D |
| doi_str_mv |
10.1002/2015WR018209 |
| dewey-full |
550 |
| title_sort |
hydrological drivers of record‐setting water level rise on earth's largest lake system |
| title_auth |
Hydrological drivers of record‐setting water level rise on Earth's largest lake system |
| abstract |
Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels |
| abstractGer |
Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels |
| abstract_unstemmed |
Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_4219 |
| container_issue |
5 |
| title_short |
Hydrological drivers of record‐setting water level rise on Earth's largest lake system |
| url |
http://dx.doi.org/10.1002/2015WR018209 http://onlinelibrary.wiley.com/doi/10.1002/2015WR018209/abstract http://search.proquest.com/docview/1798180315 |
| remote_bool |
false |
| author2 |
Bruxer, J Durnford, D Smith, J. P Clites, A. H Seglenieks, F Qian, S. S Hunter, T. S Fortin, V |
| author2Str |
Bruxer, J Durnford, D Smith, J. P Clites, A. H Seglenieks, F Qian, S. S Hunter, T. S Fortin, V |
| ppnlink |
129088285 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth oth oth oth oth oth |
| doi_str |
10.1002/2015WR018209 |
| up_date |
2024-07-03T18:22:50.599Z |
| _version_ |
1803583195029962752 |
| 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">OLC1977463010</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220221191544.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">160719s2016 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1002/2015WR018209</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20160719</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1977463010</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1977463010</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p962-5a5166a5bd9e657206aa489a74f9228d83dd52cafafecae3b3eafd61fabc7ddf0</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0046260820160000052000504026hydrologicaldriversofrecordsettingwaterlevelriseon</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">DNB</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.85</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Gronewold, A. D</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Hydrological drivers of record‐setting water level rise on Earth's largest lake system</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</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">Between January 2013 and December 2014, water levels on Lake Superior and Lake Michigan‐Huron, the two largest lakes on Earth by surface area, rose at the highest rate ever recorded for a 2 year period beginning in January and ending in December of the following year. This historic event coincided with below‐average air temperatures and extensive winter ice cover across the Great Lakes. It also brought an end to a 15 year period of persistently below‐average water levels on Lakes Superior and Michigan‐Huron that included several months of record‐low water levels. To differentiate hydrological drivers behind the recent water level rise, we developed a Bayesian Markov chain Monte Carlo (MCMC) routine for inferring historical estimates of the major components of each lake's water budget. Our results indicate that, in 2013, the water level rise on Lake Superior was driven by increased spring runoff and over‐lake precipitation. In 2014, reduced over‐lake evaporation played a more significant role in Lake Superior's water level rise. The water level rise on Lake Michigan‐Huron in 2013 was also due to above‐average spring runoff and persistent over‐lake precipitation, while in 2014, it was due to a rare combination of below‐average evaporation, above‐average runoff and precipitation, and very high inflow rates from Lake Superior through the St. Marys River. We expect, in future research, to apply our new framework across the other Laurentian Great Lakes, and to Earth's other large freshwater basins as well. Between January 2013 and December 2014, the two largest lakes on Earth rose at a record‐setting rate We developed a Bayesian MCMC routine for inferring estimates of the water budget for this period The cold 2013–2014 winter contributed to reduced evaporation rates and rising water levels</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: © 2016. American Geophysical Union. All Rights Reserved.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Bayesian</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Great Lakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">water balance</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">hydrological cycle</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Hydrology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Lakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Precipitation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Runoff</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bruxer, J</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Durnford, D</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Smith, J. P</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Clites, A. H</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Seglenieks, F</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Qian, S. S</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Hunter, T. S</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fortin, V</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Water resources research</subfield><subfield code="d">Hoboken, NJ : Wiley, 1965</subfield><subfield code="g">52(2016), 5, Seite 4026-4042</subfield><subfield code="w">(DE-627)129088285</subfield><subfield code="w">(DE-600)5564-5</subfield><subfield code="w">(DE-576)014422980</subfield><subfield code="x">0043-1397</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:52</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:5</subfield><subfield code="g">pages:4026-4042</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1002/2015WR018209</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://onlinelibrary.wiley.com/doi/10.1002/2015WR018209/abstract</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1798180315</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_4219</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.85</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">52</subfield><subfield code="j">2016</subfield><subfield code="e">5</subfield><subfield code="h">4026-4042</subfield></datafield></record></collection>
|
| score |
7.4000416 |