Class information for: |
Basic class information |
Class id | #P | Avg. number of references |
Database coverage of references |
---|---|---|---|
19302 | 512 | 31.9 | 46% |
Hierarchy of classes |
The table includes all classes above and classes immediately below the current class. |
Cluster id | Level | Cluster label | #P |
---|---|---|---|
4 | 4 | ENVIRONMENTAL SCIENCES//GEOSCIENCES, MULTIDISCIPLINARY//METEOROLOGY & ATMOSPHERIC SCIENCES | 1766162 |
524 | 3 | JOURNAL OF GLACIOLOGY//COLD REGIONS SCIENCE AND TECHNOLOGY//ANNALS OF GLACIOLOGY | 20397 |
448 | 2 | JOURNAL OF GLACIOLOGY//ANNALS OF GLACIOLOGY//CRYOSPHERE | 16162 |
19302 | 1 | JOURNAL OF GLACIOLOGY//ICE CRYSTAL STUDIES//CONTINUOUS DIVERSITY | 512 |
Terms with highest relevance score |
rank | Term | termType | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|---|
1 | JOURNAL OF GLACIOLOGY | journal | 300712 | 22% | 5% | 112 |
2 | ICE CRYSTAL STUDIES | authKW | 268369 | 1% | 75% | 6 |
3 | CONTINUOUS DIVERSITY | authKW | 248491 | 1% | 83% | 5 |
4 | ANISOTROPIC ICE FLOW | authKW | 178915 | 1% | 100% | 3 |
5 | POLAR ICE | authKW | 165940 | 2% | 35% | 8 |
6 | FABRIC ANALYSER | authKW | 134185 | 1% | 75% | 3 |
7 | ICE RHEOLOGY | authKW | 127046 | 1% | 30% | 7 |
8 | ICE FABRIC | authKW | 119277 | 0% | 100% | 2 |
9 | MIGRATION RECRYSTALLIZATION | authKW | 119277 | 0% | 100% | 2 |
10 | ANNALS OF GLACIOLOGY | journal | 110032 | 11% | 3% | 55 |
Web of Science journal categories |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|
1 | Geography, Physical | 13876 | 28% | 0% | 142 |
2 | Geosciences, Multidisciplinary | 9558 | 50% | 0% | 256 |
3 | Geochemistry & Geophysics | 585 | 10% | 0% | 51 |
4 | Microscopy | 452 | 3% | 0% | 17 |
5 | Metallurgy & Metallurgical Engineering | 303 | 9% | 0% | 46 |
6 | Engineering, Environmental | 181 | 5% | 0% | 27 |
7 | Engineering, Civil | 146 | 5% | 0% | 27 |
8 | Materials Science, Multidisciplinary | 128 | 14% | 0% | 73 |
9 | Physics, Multidisciplinary | 69 | 7% | 0% | 36 |
10 | Physics, Condensed Matter | 63 | 8% | 0% | 41 |
Address terms |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|
1 | GLACIOL GEOPHYS ENVIRONM | 109611 | 8% | 5% | 39 |
2 | AWI GLACIOL | 59638 | 0% | 100% | 1 |
3 | FRE 2192 | 59638 | 0% | 100% | 1 |
4 | GEODES GEOPHYS | 59638 | 0% | 100% | 1 |
5 | GZG SECT CRYSTALLOG | 59638 | 0% | 100% | 1 |
6 | ICE CLIMAGE GRP | 59638 | 0% | 100% | 1 |
7 | IST ITALIANO AFRICA ORIENTE | 59638 | 0% | 100% | 1 |
8 | MAT STRUTTURE INTELLIGENTI | 59638 | 0% | 100% | 1 |
9 | OFF CENT REG GEOLOGIST | 59638 | 0% | 100% | 1 |
10 | OFF REG GEOL | 59638 | 0% | 100% | 1 |
Journals |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|
1 | JOURNAL OF GLACIOLOGY | 300712 | 22% | 5% | 112 |
2 | ANNALS OF GLACIOLOGY | 110032 | 11% | 3% | 55 |
3 | ANNALS OF GLACIOLOGY-SERIES | 24667 | 1% | 7% | 6 |
4 | COLD REGIONS SCIENCE AND TECHNOLOGY | 20159 | 5% | 1% | 27 |
5 | CONTINUUM MECHANICS AND THERMODYNAMICS | 4438 | 2% | 1% | 8 |
6 | PHILOSOPHICAL MAGAZINE A-PHYSICS OF CONDENSED MATTER STRUCTURE DEFECTS AND MECHANICAL PROPERTIES | 4183 | 3% | 0% | 16 |
7 | CRYOSPHERE | 3985 | 2% | 1% | 8 |
8 | PETERMANNS GEOGRAPHISCHE MITTEILUNGEN | 2870 | 0% | 2% | 2 |
9 | JOURNAL OF STRUCTURAL GEOLOGY | 2048 | 2% | 0% | 12 |
10 | JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH | 1406 | 3% | 0% | 16 |
Author Key Words |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
LCSH search | Wikipedia search |
---|---|---|---|---|---|---|---|
1 | ICE CRYSTAL STUDIES | 268369 | 1% | 75% | 6 | Search ICE+CRYSTAL+STUDIES | Search ICE+CRYSTAL+STUDIES |
2 | CONTINUOUS DIVERSITY | 248491 | 1% | 83% | 5 | Search CONTINUOUS+DIVERSITY | Search CONTINUOUS+DIVERSITY |
3 | ANISOTROPIC ICE FLOW | 178915 | 1% | 100% | 3 | Search ANISOTROPIC+ICE+FLOW | Search ANISOTROPIC+ICE+FLOW |
4 | POLAR ICE | 165940 | 2% | 35% | 8 | Search POLAR+ICE | Search POLAR+ICE |
5 | FABRIC ANALYSER | 134185 | 1% | 75% | 3 | Search FABRIC+ANALYSER | Search FABRIC+ANALYSER |
6 | ICE RHEOLOGY | 127046 | 1% | 30% | 7 | Search ICE+RHEOLOGY | Search ICE+RHEOLOGY |
7 | ICE FABRIC | 119277 | 0% | 100% | 2 | Search ICE+FABRIC | Search ICE+FABRIC |
8 | MIGRATION RECRYSTALLIZATION | 119277 | 0% | 100% | 2 | Search MIGRATION+RECRYSTALLIZATION | Search MIGRATION+RECRYSTALLIZATION |
9 | ICE MICROSTRUCTURE | 107347 | 1% | 60% | 3 | Search ICE+MICROSTRUCTURE | Search ICE+MICROSTRUCTURE |
10 | ICE | 82824 | 9% | 3% | 46 | Search ICE | Search ICE |
Core articles |
The table includes core articles in the class. The following variables is taken into account for the relevance score of an article in a cluster c: (1) Number of references referring to publications in the class. (2) Share of total number of active references referring to publications in the class. (3) Age of the article. New articles get higher score than old articles. (4) Citation rate, normalized to year. |
Rank | Reference | # ref. in cl. |
Shr. of ref. in cl. |
Citations |
---|---|---|---|---|
1 | FARIA, SH , WEIKUSAT, I , AZUMA, N , (2014) THE MICROSTRUCTURE OF POLAR ICE. PART II: STATE OF THE ART.JOURNAL OF STRUCTURAL GEOLOGY. VOL. 61. ISSUE . P. 21 -49 | 85 | 68% | 11 |
2 | WEIKUSAT, I , JANSEN, D , BINDER, T , EICHLER, J , FARIA, SH , WILHELMS, F , KIPFSTUHL, S , SHELDON, S , MILLER, H , DAHL-JENSEN, D , ET AL (2017) PHYSICAL ANALYSIS OF AN ANTARCTIC ICE CORE-TOWARDS AN INTEGRATION OF MICRO- AND MACRODYNAMICS OF POLAR ICE.PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES. VOL. 375. ISSUE 2086. P. - | 37 | 53% | 2 |
3 | LLORENS, MG , GRIERA, A , STEINBACH, F , BONS, PD , GOMEZ-RIVAS, E , JANSEN, D , ROESSIGER, J , LEBENSOHN, RA , WEIKUSAT, I , (2017) DYNAMIC RECRYSTALLIZATION DURING DEFORMATION OF POLYCRYSTALLINE ICE: INSIGHTS FROM NUMERICAL SIMULATIONS.PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES. VOL. 375. ISSUE 2086. P. - | 32 | 60% | 2 |
4 | MONTAGNAT, M , CASTELNAU, O , BONS, PD , FARIA, SH , GAGLIARDINI, O , GILLET-CHAULET, F , GRENNERAT, F , GRIERA, A , LEBENSOHN, RA , MOULINEC, H , ET AL (2014) MULTISCALE MODELING OF ICE DEFORMATION BEHAVIOR.JOURNAL OF STRUCTURAL GEOLOGY. VOL. 61. ISSUE . P. 78 -108 | 71 | 45% | 17 |
5 | CHAUVE, T , MONTAGNAT, M , BAROU, F , HIDAS, K , TOMMASI, A , MAINPRICE, D , (2017) INVESTIGATION OF NUCLEATION PROCESSES DURING DYNAMIC RECRYSTALLIZATION OF ICE USING CRYO-EBSD.PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES. VOL. 375. ISSUE 2086. P. - | 32 | 49% | 2 |
6 | TREVERROW, A , BUDD, WF , JACKA, TH , WARNER, RC , (2012) THE TERTIARY CREEP OF POLYCRYSTALLINE ICE: EXPERIMENTAL EVIDENCE FOR STRESS-DEPENDENT LEVELS OF STRAIN-RATE ENHANCEMENT.JOURNAL OF GLACIOLOGY. VOL. 58. ISSUE 208. P. 301 -314 | 36 | 88% | 10 |
7 | TREVERROW, A , WARNER, RC , BUDD, WF , JACKA, TH , ROBERTS, JL , (2015) MODELLED STRESS DISTRIBUTIONS AT THE DOME SUMMIT SOUTH BOREHOLE, LAW DOME, EAST ANTARCTICA: A COMPARISON OF ANISOTROPIC ICE FLOW RELATIONS.JOURNAL OF GLACIOLOGY. VOL. 61. ISSUE 229. P. 987 -1004 | 39 | 72% | 0 |
8 | WEIKUSAT, I , KIPFSTUHL, S , FARIA, SH , AZUMA, N , MIYAMOTO, A , (2009) SUBGRAIN BOUNDARIES AND RELATED MICROSTRUCTURAL FEATURES IN EDML (ANTARCTICA) DEEP ICE CORE.JOURNAL OF GLACIOLOGY. VOL. 55. ISSUE 191. P. 461 -472 | 39 | 76% | 15 |
9 | KENNEDY, JH , PETTIT, EC , (2015) THE RESPONSE OF FABRIC VARIATIONS TO SIMPLE SHEAR AND MIGRATION RECRYSTALLIZATION.JOURNAL OF GLACIOLOGY. VOL. 61. ISSUE 227. P. 537 -550 | 33 | 80% | 0 |
10 | DIPRINZIO, CL , WILEN, LA , ALLEY, RB , FITZPATRICK, JJ , SPENCER, MK , GOW, AJ , (2005) FABRIC AND TEXTURE AT SIPLE DOME, ANTARCTICA.JOURNAL OF GLACIOLOGY. VOL. 51. ISSUE 173. P. 281 -290 | 33 | 92% | 27 |
Classes with closest relation at Level 1 |