Class information for: |
Basic class information |
Class id | #P | Avg. number of references |
Database coverage of references |
---|---|---|---|
15111 | 731 | 22.5 | 41% |
Hierarchy of classes |
The table includes all classes above and classes immediately below the current class. |
Cluster id | Level | Cluster label | #P |
---|---|---|---|
15 | 4 | MATHEMATICS//MATHEMATICS, APPLIED//MATH | 719832 |
244 | 3 | MATHEMATICS, APPLIED//MATHEMATICS//BLOW UP | 46988 |
704 | 2 | NAVIER STOKES EQUATIONS//GLOBAL ATTRACTOR//CAHN HILLIARD EQUATION | 12952 |
15111 | 1 | PRIMITIVE EQUATIONS//SCI COMP PL MATH//PL MATH SCI COMP | 731 |
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 | PRIMITIVE EQUATIONS | authKW | 1801470 | 9% | 65% | 66 |
2 | SCI COMP PL MATH | address | 1588998 | 9% | 57% | 67 |
3 | PL MATH SCI COMP | address | 443677 | 5% | 30% | 36 |
4 | PRANDTL EQUATIONS | authKW | 421186 | 2% | 92% | 11 |
5 | HYDROSTATIC APPROXIMATION | authKW | 334157 | 2% | 67% | 12 |
6 | MATH CALCUL SCI | address | 208853 | 1% | 100% | 5 |
7 | NONVISCOUS PRIMITIVE EQUATIONS | authKW | 208853 | 1% | 100% | 5 |
8 | PRIMITIVE EQUATIONS FOR THE OCEAN | authKW | 167083 | 1% | 100% | 4 |
9 | QUASIGEOSTROPHIC FLUID MODEL | authKW | 167083 | 1% | 100% | 4 |
10 | INVISCID LIMIT | authKW | 164488 | 2% | 25% | 16 |
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 | Mathematics, Applied | 18550 | 63% | 0% | 458 |
2 | Mathematics | 7678 | 44% | 0% | 325 |
3 | Physics, Mathematical | 831 | 10% | 0% | 73 |
4 | Mechanics | 690 | 11% | 0% | 84 |
5 | Physics, Fluids & Plasmas | 285 | 5% | 0% | 39 |
6 | Mathematics, Interdisciplinary Applications | 220 | 4% | 0% | 32 |
7 | Computer Science, Interdisciplinary Applications | 32 | 2% | 0% | 18 |
8 | Engineering, General | 24 | 2% | 0% | 14 |
9 | Meteorology & Atmospheric Sciences | 4 | 1% | 0% | 10 |
10 | Oceanography | 3 | 1% | 0% | 7 |
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 | SCI COMP PL MATH | 1588998 | 9% | 57% | 67 |
2 | PL MATH SCI COMP | 443677 | 5% | 30% | 36 |
3 | MATH CALCUL SCI | 208853 | 1% | 100% | 5 |
4 | ETSE CAMINOS | 83541 | 0% | 100% | 2 |
5 | EDAN IMUS | 75185 | 0% | 60% | 3 |
6 | URA 2053 | 62012 | 1% | 21% | 7 |
7 | CNRS 8050 | 55693 | 0% | 67% | 2 |
8 | ANAL NUMER | 53894 | 4% | 4% | 31 |
9 | BUDGET TREASURY | 41771 | 0% | 100% | 1 |
10 | DEP ECUAC DIFERENCIALES ANAL NUMER | 41771 | 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 MATHEMATICAL FLUID MECHANICS | 31366 | 2% | 4% | 18 |
2 | ASYMPTOTIC ANALYSIS | 11424 | 2% | 2% | 18 |
3 | COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE I-MATHEMATIQUE | 9945 | 6% | 1% | 45 |
4 | INTERNATIONAL JOURNAL OF NUMERICAL ANALYSIS AND MODELING | 9812 | 2% | 2% | 11 |
5 | NONLINEARITY | 8001 | 3% | 1% | 25 |
6 | SIAM JOURNAL ON MATHEMATICAL ANALYSIS | 6499 | 3% | 1% | 24 |
7 | ARCHIVE FOR RATIONAL MECHANICS AND ANALYSIS | 5890 | 3% | 1% | 19 |
8 | ANALYSIS AND APPLICATIONS | 4615 | 1% | 2% | 6 |
9 | DISCRETE AND CONTINUOUS DYNAMICAL SYSTEMS | 4495 | 3% | 1% | 19 |
10 | COMMUNICATIONS ON PURE AND APPLIED MATHEMATICS | 4397 | 2% | 1% | 13 |
Author Key Words |
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 | KUKAVICA, I , LOMBARDO, MC , SAMMARTINO, M , (2016) ZERO VISCOSITY LIMIT FOR ANALYTIC SOLUTIONS OF THE PRIMITIVE EQUATIONS.ARCHIVE FOR RATIONAL MECHANICS AND ANALYSIS. VOL. 222. ISSUE 1. P. 15 -45 | 43 | 100% | 0 |
2 | FEI, MW , HAN, DZ , WANG, XM , (2017) INITIAL-BOUNDARY LAYER ASSOCIATED WITH THE NONLINEAR DARCY-BRINKMAN-OBERBECK-BOUSSINESQ SYSTEM.PHYSICA D-NONLINEAR PHENOMENA. VOL. 338. ISSUE . P. 42 -56 | 45 | 83% | 0 |
3 | KUKAVICA, I , MASMOUDI, N , VICOL, V , WONG, TK , (2014) ON THE LOCAL WELL-POSEDNESS OF THE PRANDTL AND HYDROSTATIC EULER EQUATIONS WITH MULTIPLE MONOTONICITY REGIONS.SIAM JOURNAL ON MATHEMATICAL ANALYSIS. VOL. 46. ISSUE 6. P. 3865 -3890 | 41 | 89% | 4 |
4 | GIE, GM , JUNG, CY , TEMAM, R , (2016) RECENT PROGRESSES IN BOUNDARY LAYER THEORY.DISCRETE AND CONTINUOUS DYNAMICAL SYSTEMS. VOL. 36. ISSUE 5. P. 2521 -2583 | 52 | 60% | 1 |
5 | HAN, DZ , WANG, XM , (2014) INITIAL-BOUNDARY LAYER ASSOCIATED WITH THE NONLINEAR DARCY-BRINKMAN SYSTEM.JOURNAL OF DIFFERENTIAL EQUATIONS. VOL. 256. ISSUE 2. P. 609 -639 | 38 | 83% | 1 |
6 | CANNONE, M , LOMBARDO, MC , SAMMARTINO, M , (2014) ON THE PRANDTL BOUNDARY LAYER EQUATIONS IN PRESENCE OF CORNER SINGULARITIES.ACTA APPLICANDAE MATHEMATICAE. VOL. 132. ISSUE 1. P. 139 -149 | 31 | 91% | 1 |
7 | CANNONE, M , LOMBARDO, MC , SAMMARTINO, M , (2013) WELL-POSEDNESS OF PRANDTL EQUATIONS WITH NON-COMPATIBLE DATA.NONLINEARITY. VOL. 26. ISSUE 12. P. 3077 -3100 | 33 | 80% | 5 |
8 | MASMOUDI, N , WONG, TK , (2015) LOCAL-IN-TIME EXISTENCE AND UNIQUENESS OF SOLUTIONS TO THE PRANDTL EQUATIONS BY ENERGY METHODS.COMMUNICATIONS ON PURE AND APPLIED MATHEMATICS. VOL. 68. ISSUE 10. P. 1683 -1741 | 23 | 100% | 7 |
9 | HAN, DZ , MAZZUCATO, AL , NIU, DJ , WANG, XM , (2012) BOUNDARY LAYER FOR A CLASS OF NONLINEAR PIPE FLOW.JOURNAL OF DIFFERENTIAL EQUATIONS. VOL. 252. ISSUE 12. P. 6387 -6413 | 27 | 100% | 4 |
10 | KELLIHER, JP , TEMAM, R , WANG, XM , (2011) BOUNDARY LAYER ASSOCIATED WITH THE DARCY-BRINKMAN-BOUSSINESQ MODEL FOR CONVECTION IN POROUS MEDIA.PHYSICA D-NONLINEAR PHENOMENA. VOL. 240. ISSUE 7. P. 619 -628 | 34 | 79% | 11 |
Classes with closest relation at Level 1 |