Class information for: |
Basic class information |
Hierarchy of classes |
The table includes all classes above and classes immediately below the current class. |
| Cluster id | Level | Cluster label | #P |
|---|---|---|---|
| 21 | 4 | THERMODYNAMICS//MECHANICS//ENGINEERING, MECHANICAL | 471779 |
| 578 | 3 | GEOPHYSICAL AND ASTROPHYSICAL FLUID DYNAMICS//GEODYNAMO//PHYSICS, FLUIDS & PLASMAS | 16221 |
| 1290 | 2 | PHYSICS, FLUIDS & PLASMAS//JOURNAL OF THE ATMOSPHERIC SCIENCES//JOURNAL OF FLUID MECHANICS | 9013 |
| 14799 | 1 | JOURNAL OF THE ATMOSPHERIC SCIENCES//ZONAL JETS//RHINES SCALE | 776 |
Terms with highest relevance score |
| rank | Category | termType | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|---|
| 1 | JOURNAL OF THE ATMOSPHERIC SCIENCES | journal | 279734 | 32% | 3% | 246 |
| 2 | ZONAL JETS | authKW | 270747 | 1% | 67% | 10 |
| 3 | RHINES SCALE | authKW | 169219 | 1% | 83% | 5 |
| 4 | GEOL MUSEUM 452 | address | 129960 | 1% | 80% | 4 |
| 5 | PERLSTONE AERONAUT ENGN STUDIES | address | 129952 | 1% | 40% | 8 |
| 6 | AXISYMMETRIC TO NONAXISYMMETRIC TRANSITION | authKW | 121839 | 0% | 100% | 3 |
| 7 | DIFFERENTIALLY HEATED ROTATING FLUID EXPERIMENT | authKW | 121839 | 0% | 100% | 3 |
| 8 | DRIFT WAVES IN PLASMAS | authKW | 121839 | 0% | 100% | 3 |
| 9 | NUMERICAL APPROXIMATION OF NORMAL FORM COEFFICIENTS | authKW | 121839 | 0% | 100% | 3 |
| 10 | TRIAD RESONANCES | authKW | 121839 | 0% | 100% | 3 |
Web of Science journal categories |
| chi_square_rank | Category | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|
| 1 | Meteorology & Atmospheric Sciences | 23773 | 49% | 0% | 380 |
| 2 | Oceanography | 3442 | 15% | 0% | 118 |
| 3 | Mechanics | 2182 | 19% | 0% | 148 |
| 4 | Physics, Fluids & Plasmas | 2152 | 13% | 0% | 103 |
| 5 | Geochemistry & Geophysics | 990 | 10% | 0% | 81 |
| 6 | Physics, Mathematical | 321 | 6% | 0% | 49 |
| 7 | Physics, Multidisciplinary | 183 | 9% | 0% | 67 |
| 8 | Mathematics, Applied | 110 | 6% | 0% | 47 |
| 9 | Astronomy & Astrophysics | 62 | 5% | 0% | 40 |
| 10 | Geosciences, Multidisciplinary | 50 | 4% | 0% | 32 |
Address terms |
| chi_square_rank | term | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|
| 1 | GEOL MUSEUM 452 | 129960 | 1% | 80% | 4 |
| 2 | PERLSTONE AERONAUT ENGN STUDIES | 129952 | 1% | 40% | 8 |
| 3 | LEHRSTUHL AERODYNAM STROMUNGSLEHRE | 54149 | 0% | 67% | 2 |
| 4 | ATMOSPHER CHEM BRANCH 964 | 40613 | 0% | 100% | 1 |
| 5 | CNRS IRD UBO UMR6523 | 40613 | 0% | 100% | 1 |
| 6 | CNRSECOLE POLYTECHUMR8539 | 40613 | 0% | 100% | 1 |
| 7 | CR CASACCRA | 40613 | 0% | 100% | 1 |
| 8 | CYPRUS OCEANOG | 40613 | 0% | 100% | 1 |
| 9 | DYNAM BRANCH | 40613 | 0% | 100% | 1 |
| 10 | EARTH PLANET SPACE SCI | 40613 | 0% | 100% | 1 |
Journals |
| chi_square_rank | term | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|
| 1 | JOURNAL OF THE ATMOSPHERIC SCIENCES | 279734 | 32% | 3% | 246 |
| 2 | GEOPHYSICAL AND ASTROPHYSICAL FLUID DYNAMICS | 32312 | 4% | 2% | 34 |
| 3 | JOURNAL OF PHYSICAL OCEANOGRAPHY | 18052 | 7% | 1% | 53 |
| 4 | DYNAMICS OF ATMOSPHERES AND OCEANS | 13808 | 2% | 2% | 17 |
| 5 | NONLINEAR PROCESSES IN GEOPHYSICS | 9587 | 2% | 1% | 17 |
| 6 | JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN | 9023 | 3% | 1% | 24 |
| 7 | JOURNAL OF FLUID MECHANICS | 4288 | 5% | 0% | 41 |
| 8 | QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY | 2501 | 2% | 0% | 17 |
| 9 | PHYSICS OF FLUIDS | 2480 | 4% | 0% | 30 |
| 10 | JOURNAL OF MARINE RESEARCH | 1884 | 1% | 1% | 8 |
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. |
Classes with closest relation at Level 1 |