Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP)
Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated cli...
Ausführliche Beschreibung
Autor*in: |
Mearns, L. O. [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2013 |
---|
Schlagwörter: |
Regional Climate Model Simulation Canadian Regional Climate Model |
---|
Systematik: |
|
---|
Anmerkung: |
© The Author(s) 2013 |
---|
Übergeordnetes Werk: |
Enthalten in: Climatic change - Springer Netherlands, 1977, 120(2013), 4 vom: 27. Juli, Seite 965-975 |
---|---|
Übergeordnetes Werk: |
volume:120 ; year:2013 ; number:4 ; day:27 ; month:07 ; pages:965-975 |
Links: |
---|
DOI / URN: |
10.1007/s10584-013-0831-3 |
---|
Katalog-ID: |
OLC2062612206 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | OLC2062612206 | ||
003 | DE-627 | ||
005 | 20230503024255.0 | ||
007 | tu | ||
008 | 200819s2013 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1007/s10584-013-0831-3 |2 doi | |
035 | |a (DE-627)OLC2062612206 | ||
035 | |a (DE-He213)s10584-013-0831-3-p | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 550 |q VZ |
084 | |a 14 |2 ssgn | ||
084 | |a RA 1000 |q VZ |2 rvk | ||
100 | 1 | |a Mearns, L. O. |e verfasserin |4 aut | |
245 | 1 | 0 | |a Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) |
264 | 1 | |c 2013 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
500 | |a © The Author(s) 2013 | ||
520 | |a Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs. | ||
650 | 4 | |a Regional Climate Model | |
650 | 4 | |a Regional Climate Model Simulation | |
650 | 4 | |a Canadian Regional Climate Model | |
650 | 4 | |a North American Regional Climate Change Assessment Program | |
650 | 4 | |a Regional Spectral Model | |
700 | 1 | |a Sain, S. |4 aut | |
700 | 1 | |a Leung, L. R. |4 aut | |
700 | 1 | |a Bukovsky, M. S. |4 aut | |
700 | 1 | |a McGinnis, S. |4 aut | |
700 | 1 | |a Biner, S. |4 aut | |
700 | 1 | |a Caya, D. |4 aut | |
700 | 1 | |a Arritt, R. W. |4 aut | |
700 | 1 | |a Gutowski, W. |4 aut | |
700 | 1 | |a Takle, E. |4 aut | |
700 | 1 | |a Snyder, M. |4 aut | |
700 | 1 | |a Jones, R. G. |4 aut | |
700 | 1 | |a Nunes, A. M. B. |4 aut | |
700 | 1 | |a Tucker, S. |4 aut | |
700 | 1 | |a Herzmann, D. |4 aut | |
700 | 1 | |a McDaniel, L. |4 aut | |
700 | 1 | |a Sloan, L. |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Climatic change |d Springer Netherlands, 1977 |g 120(2013), 4 vom: 27. Juli, Seite 965-975 |w (DE-627)130479020 |w (DE-600)751086-X |w (DE-576)016068610 |x 0165-0009 |7 nnns |
773 | 1 | 8 | |g volume:120 |g year:2013 |g number:4 |g day:27 |g month:07 |g pages:965-975 |
856 | 4 | 1 | |u https://doi.org/10.1007/s10584-013-0831-3 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a SSG-OLC-UMW | ||
912 | |a SSG-OLC-GEO | ||
912 | |a SSG-OLC-IBL | ||
912 | |a SSG-OPC-GGO | ||
912 | |a GBV_ILN_11 | ||
912 | |a GBV_ILN_40 | ||
912 | |a GBV_ILN_62 | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_154 | ||
912 | |a GBV_ILN_601 | ||
912 | |a GBV_ILN_4012 | ||
912 | |a GBV_ILN_4325 | ||
936 | r | v | |a RA 1000 |
951 | |a AR | ||
952 | |d 120 |j 2013 |e 4 |b 27 |c 07 |h 965-975 |
author_variant |
l o m lo lom s s ss l r l lr lrl m s b ms msb s m sm s b sb d c dc r w a rw rwa w g wg e t et m s ms r g j rg rgj a m b n amb ambn s t st d h dh l m lm l s ls |
---|---|
matchkey_str |
article:01650009:2013----::lmtcagpoetosfhnrhmrcneinllmtcag |
hierarchy_sort_str |
2013 |
publishDate |
2013 |
allfields |
10.1007/s10584-013-0831-3 doi (DE-627)OLC2062612206 (DE-He213)s10584-013-0831-3-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Mearns, L. O. verfasserin aut Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2013 Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs. Regional Climate Model Regional Climate Model Simulation Canadian Regional Climate Model North American Regional Climate Change Assessment Program Regional Spectral Model Sain, S. aut Leung, L. R. aut Bukovsky, M. S. aut McGinnis, S. aut Biner, S. aut Caya, D. aut Arritt, R. W. aut Gutowski, W. aut Takle, E. aut Snyder, M. aut Jones, R. G. aut Nunes, A. M. B. aut Tucker, S. aut Herzmann, D. aut McDaniel, L. aut Sloan, L. aut Enthalten in Climatic change Springer Netherlands, 1977 120(2013), 4 vom: 27. Juli, Seite 965-975 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:120 year:2013 number:4 day:27 month:07 pages:965-975 https://doi.org/10.1007/s10584-013-0831-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4325 RA 1000 AR 120 2013 4 27 07 965-975 |
spelling |
10.1007/s10584-013-0831-3 doi (DE-627)OLC2062612206 (DE-He213)s10584-013-0831-3-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Mearns, L. O. verfasserin aut Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2013 Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs. Regional Climate Model Regional Climate Model Simulation Canadian Regional Climate Model North American Regional Climate Change Assessment Program Regional Spectral Model Sain, S. aut Leung, L. R. aut Bukovsky, M. S. aut McGinnis, S. aut Biner, S. aut Caya, D. aut Arritt, R. W. aut Gutowski, W. aut Takle, E. aut Snyder, M. aut Jones, R. G. aut Nunes, A. M. B. aut Tucker, S. aut Herzmann, D. aut McDaniel, L. aut Sloan, L. aut Enthalten in Climatic change Springer Netherlands, 1977 120(2013), 4 vom: 27. Juli, Seite 965-975 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:120 year:2013 number:4 day:27 month:07 pages:965-975 https://doi.org/10.1007/s10584-013-0831-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4325 RA 1000 AR 120 2013 4 27 07 965-975 |
allfields_unstemmed |
10.1007/s10584-013-0831-3 doi (DE-627)OLC2062612206 (DE-He213)s10584-013-0831-3-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Mearns, L. O. verfasserin aut Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2013 Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs. Regional Climate Model Regional Climate Model Simulation Canadian Regional Climate Model North American Regional Climate Change Assessment Program Regional Spectral Model Sain, S. aut Leung, L. R. aut Bukovsky, M. S. aut McGinnis, S. aut Biner, S. aut Caya, D. aut Arritt, R. W. aut Gutowski, W. aut Takle, E. aut Snyder, M. aut Jones, R. G. aut Nunes, A. M. B. aut Tucker, S. aut Herzmann, D. aut McDaniel, L. aut Sloan, L. aut Enthalten in Climatic change Springer Netherlands, 1977 120(2013), 4 vom: 27. Juli, Seite 965-975 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:120 year:2013 number:4 day:27 month:07 pages:965-975 https://doi.org/10.1007/s10584-013-0831-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4325 RA 1000 AR 120 2013 4 27 07 965-975 |
allfieldsGer |
10.1007/s10584-013-0831-3 doi (DE-627)OLC2062612206 (DE-He213)s10584-013-0831-3-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Mearns, L. O. verfasserin aut Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2013 Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs. Regional Climate Model Regional Climate Model Simulation Canadian Regional Climate Model North American Regional Climate Change Assessment Program Regional Spectral Model Sain, S. aut Leung, L. R. aut Bukovsky, M. S. aut McGinnis, S. aut Biner, S. aut Caya, D. aut Arritt, R. W. aut Gutowski, W. aut Takle, E. aut Snyder, M. aut Jones, R. G. aut Nunes, A. M. B. aut Tucker, S. aut Herzmann, D. aut McDaniel, L. aut Sloan, L. aut Enthalten in Climatic change Springer Netherlands, 1977 120(2013), 4 vom: 27. Juli, Seite 965-975 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:120 year:2013 number:4 day:27 month:07 pages:965-975 https://doi.org/10.1007/s10584-013-0831-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4325 RA 1000 AR 120 2013 4 27 07 965-975 |
allfieldsSound |
10.1007/s10584-013-0831-3 doi (DE-627)OLC2062612206 (DE-He213)s10584-013-0831-3-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Mearns, L. O. verfasserin aut Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2013 Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs. Regional Climate Model Regional Climate Model Simulation Canadian Regional Climate Model North American Regional Climate Change Assessment Program Regional Spectral Model Sain, S. aut Leung, L. R. aut Bukovsky, M. S. aut McGinnis, S. aut Biner, S. aut Caya, D. aut Arritt, R. W. aut Gutowski, W. aut Takle, E. aut Snyder, M. aut Jones, R. G. aut Nunes, A. M. B. aut Tucker, S. aut Herzmann, D. aut McDaniel, L. aut Sloan, L. aut Enthalten in Climatic change Springer Netherlands, 1977 120(2013), 4 vom: 27. Juli, Seite 965-975 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:120 year:2013 number:4 day:27 month:07 pages:965-975 https://doi.org/10.1007/s10584-013-0831-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4325 RA 1000 AR 120 2013 4 27 07 965-975 |
language |
English |
source |
Enthalten in Climatic change 120(2013), 4 vom: 27. Juli, Seite 965-975 volume:120 year:2013 number:4 day:27 month:07 pages:965-975 |
sourceStr |
Enthalten in Climatic change 120(2013), 4 vom: 27. Juli, Seite 965-975 volume:120 year:2013 number:4 day:27 month:07 pages:965-975 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Regional Climate Model Regional Climate Model Simulation Canadian Regional Climate Model North American Regional Climate Change Assessment Program Regional Spectral Model |
dewey-raw |
550 |
isfreeaccess_bool |
false |
container_title |
Climatic change |
authorswithroles_txt_mv |
Mearns, L. O. @@aut@@ Sain, S. @@aut@@ Leung, L. R. @@aut@@ Bukovsky, M. S. @@aut@@ McGinnis, S. @@aut@@ Biner, S. @@aut@@ Caya, D. @@aut@@ Arritt, R. W. @@aut@@ Gutowski, W. @@aut@@ Takle, E. @@aut@@ Snyder, M. @@aut@@ Jones, R. G. @@aut@@ Nunes, A. M. B. @@aut@@ Tucker, S. @@aut@@ Herzmann, D. @@aut@@ McDaniel, L. @@aut@@ Sloan, L. @@aut@@ |
publishDateDaySort_date |
2013-07-27T00:00:00Z |
hierarchy_top_id |
130479020 |
dewey-sort |
3550 |
id |
OLC2062612206 |
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">OLC2062612206</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503024255.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2013 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10584-013-0831-3</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2062612206</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s10584-013-0831-3-p</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">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RA 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Mearns, L. O.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP)</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2013</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="500" ind1=" " ind2=" "><subfield code="a">© The Author(s) 2013</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Regional Climate Model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Regional Climate Model Simulation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Canadian Regional Climate Model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">North American Regional Climate Change Assessment Program</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Regional Spectral Model</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sain, S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Leung, L. R.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bukovsky, M. S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">McGinnis, S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Biner, S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Caya, D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Arritt, R. W.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gutowski, W.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Takle, E.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Snyder, M.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jones, R. G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nunes, A. M. B.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tucker, S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Herzmann, D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">McDaniel, L.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sloan, L.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Climatic change</subfield><subfield code="d">Springer Netherlands, 1977</subfield><subfield code="g">120(2013), 4 vom: 27. Juli, Seite 965-975</subfield><subfield code="w">(DE-627)130479020</subfield><subfield code="w">(DE-600)751086-X</subfield><subfield code="w">(DE-576)016068610</subfield><subfield code="x">0165-0009</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:120</subfield><subfield code="g">year:2013</subfield><subfield code="g">number:4</subfield><subfield code="g">day:27</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:965-975</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s10584-013-0831-3</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-UMW</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-IBL</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_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_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_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">RA 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">120</subfield><subfield code="j">2013</subfield><subfield code="e">4</subfield><subfield code="b">27</subfield><subfield code="c">07</subfield><subfield code="h">965-975</subfield></datafield></record></collection>
|
author |
Mearns, L. O. |
spellingShingle |
Mearns, L. O. ddc 550 ssgn 14 rvk RA 1000 misc Regional Climate Model misc Regional Climate Model Simulation misc Canadian Regional Climate Model misc North American Regional Climate Change Assessment Program misc Regional Spectral Model Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) |
authorStr |
Mearns, L. O. |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)130479020 |
format |
Article |
dewey-ones |
550 - Earth sciences |
delete_txt_mv |
keep |
author_role |
aut aut aut aut aut aut aut aut aut aut aut aut aut aut aut aut aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
0165-0009 |
topic_title |
550 VZ 14 ssgn RA 1000 VZ rvk Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) Regional Climate Model Regional Climate Model Simulation Canadian Regional Climate Model North American Regional Climate Change Assessment Program Regional Spectral Model |
topic |
ddc 550 ssgn 14 rvk RA 1000 misc Regional Climate Model misc Regional Climate Model Simulation misc Canadian Regional Climate Model misc North American Regional Climate Change Assessment Program misc Regional Spectral Model |
topic_unstemmed |
ddc 550 ssgn 14 rvk RA 1000 misc Regional Climate Model misc Regional Climate Model Simulation misc Canadian Regional Climate Model misc North American Regional Climate Change Assessment Program misc Regional Spectral Model |
topic_browse |
ddc 550 ssgn 14 rvk RA 1000 misc Regional Climate Model misc Regional Climate Model Simulation misc Canadian Regional Climate Model misc North American Regional Climate Change Assessment Program misc Regional Spectral Model |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
hierarchy_parent_title |
Climatic change |
hierarchy_parent_id |
130479020 |
dewey-tens |
550 - Earth sciences & geology |
hierarchy_top_title |
Climatic change |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)130479020 (DE-600)751086-X (DE-576)016068610 |
title |
Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) |
ctrlnum |
(DE-627)OLC2062612206 (DE-He213)s10584-013-0831-3-p |
title_full |
Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) |
author_sort |
Mearns, L. O. |
journal |
Climatic change |
journalStr |
Climatic change |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science |
recordtype |
marc |
publishDateSort |
2013 |
contenttype_str_mv |
txt |
container_start_page |
965 |
author_browse |
Mearns, L. O. Sain, S. Leung, L. R. Bukovsky, M. S. McGinnis, S. Biner, S. Caya, D. Arritt, R. W. Gutowski, W. Takle, E. Snyder, M. Jones, R. G. Nunes, A. M. B. Tucker, S. Herzmann, D. McDaniel, L. Sloan, L. |
container_volume |
120 |
class |
550 VZ 14 ssgn RA 1000 VZ rvk |
format_se |
Aufsätze |
author-letter |
Mearns, L. O. |
doi_str_mv |
10.1007/s10584-013-0831-3 |
dewey-full |
550 |
title_sort |
climate change projections of the north american regional climate change assessment program (narccap) |
title_auth |
Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) |
abstract |
Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs. © The Author(s) 2013 |
abstractGer |
Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs. © The Author(s) 2013 |
abstract_unstemmed |
Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs. © The Author(s) 2013 |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4325 |
container_issue |
4 |
title_short |
Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP) |
url |
https://doi.org/10.1007/s10584-013-0831-3 |
remote_bool |
false |
author2 |
Sain, S. Leung, L. R. Bukovsky, M. S. McGinnis, S. Biner, S. Caya, D. Arritt, R. W. Gutowski, W. Takle, E. Snyder, M. Jones, R. G. Nunes, A. M. B. Tucker, S. Herzmann, D. McDaniel, L. Sloan, L. |
author2Str |
Sain, S. Leung, L. R. Bukovsky, M. S. McGinnis, S. Biner, S. Caya, D. Arritt, R. W. Gutowski, W. Takle, E. Snyder, M. Jones, R. G. Nunes, A. M. B. Tucker, S. Herzmann, D. McDaniel, L. Sloan, L. |
ppnlink |
130479020 |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/s10584-013-0831-3 |
up_date |
2024-07-03T15:45:55.655Z |
_version_ |
1803573322746691584 |
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">OLC2062612206</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503024255.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2013 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10584-013-0831-3</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2062612206</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s10584-013-0831-3-p</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">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RA 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Mearns, L. O.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Climate change projections of the North American Regional Climate Change Assessment Program (NARCCAP)</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2013</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="500" ind1=" " ind2=" "><subfield code="a">© The Author(s) 2013</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract We investigate major results of the NARCCAP multiple regional climate model (RCM) experiments driven by multiple global climate models (GCMs) regarding climate change for seasonal temperature and precipitation over North America. We focus on two major questions: How do the RCM simulated climate changes differ from those of the parent GCMs and thus affect our perception of climate change over North America, and how important are the relative contributions of RCMs and GCMs to the uncertainty (variance explained) for different seasons and variables? The RCMs tend to produce stronger climate changes for precipitation: larger increases in the northern part of the domain in winter and greater decreases across a swath of the central part in summer, compared to the four GCMs driving the regional models as well as to the full set of CMIP3 GCM results. We pose some possible process-level mechanisms for the difference in intensity of change, particularly for summer. Detailed process-level studies will be necessary to establish mechanisms and credibility of these results. The GCMs explain more variance for winter temperature and the RCMs for summer temperature. The same is true for precipitation patterns. Thus, we recommend that future RCM-GCM experiments over this region include a balanced number of GCMs and RCMs.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Regional Climate Model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Regional Climate Model Simulation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Canadian Regional Climate Model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">North American Regional Climate Change Assessment Program</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Regional Spectral Model</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sain, S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Leung, L. R.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bukovsky, M. S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">McGinnis, S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Biner, S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Caya, D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Arritt, R. W.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gutowski, W.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Takle, E.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Snyder, M.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jones, R. G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nunes, A. M. B.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tucker, S.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Herzmann, D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">McDaniel, L.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sloan, L.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Climatic change</subfield><subfield code="d">Springer Netherlands, 1977</subfield><subfield code="g">120(2013), 4 vom: 27. Juli, Seite 965-975</subfield><subfield code="w">(DE-627)130479020</subfield><subfield code="w">(DE-600)751086-X</subfield><subfield code="w">(DE-576)016068610</subfield><subfield code="x">0165-0009</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:120</subfield><subfield code="g">year:2013</subfield><subfield code="g">number:4</subfield><subfield code="g">day:27</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:965-975</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s10584-013-0831-3</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-UMW</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-IBL</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_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_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_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">RA 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">120</subfield><subfield code="j">2013</subfield><subfield code="e">4</subfield><subfield code="b">27</subfield><subfield code="c">07</subfield><subfield code="h">965-975</subfield></datafield></record></collection>
|
score |
7.3975716 |