| Class information for:  | 
| Basic class information | 
| ID | Publications | Average number of references | Avg. shr. active ref. in WoS | 
|---|---|---|---|
| 1854 | 2383 | 32.9 | 60% | 
| Classes in level above (level 2) | 
| ID, lev. above | Publications | Label for level above | 
|---|---|---|
| 1464 | 7222 | INTERNAL WAVES//INTERNAL TIDES//INTERNAL SOLITARY WAVES | 
| Terms with highest relevance score | 
| Rank | Term | Type of term | Relevance score (tfidf) | Class's shr. of term's tot. occurrences | Shr. of publ. in class containing term | Num. of publ. in class | 
|---|---|---|---|---|---|---|
| 1 | INTERNAL TIDES | Author keyword | 78 | 52% | 4% | 106 | 
| 2 | INTERNAL WAVES | Author keyword | 46 | 25% | 7% | 160 | 
| 3 | DIAPYCNAL MIXING | Author keyword | 18 | 48% | 1% | 27 | 
| 4 | PARAMETRIC SUBHARMONIC INSTABILITY | Author keyword | 14 | 100% | 0% | 7 | 
| 5 | BAROCLINIC TIDES | Author keyword | 9 | 67% | 0% | 8 | 
| 6 | NEAR INERTIAL WAVES | Author keyword | 8 | 70% | 0% | 7 | 
| 7 | STRATIFIED TURBULENCE | Author keyword | 8 | 30% | 1% | 23 | 
| 8 | INTERNAL WAVE BREAKING | Author keyword | 6 | 71% | 0% | 5 | 
| 9 | NEAR INERTIAL CURRENTS | Author keyword | 6 | 71% | 0% | 5 | 
| 10 | NEAR INERTIAL MOTIONS | Author keyword | 6 | 100% | 0% | 4 | 
| Web of Science journal categories | 
| Author Key Words | 
| Rank | Web of Science journal category | Relevance score (tfidf) | Class's shr. of term's tot. occurrences | Shr. of publ. in class containing term | Num. of publ. in class | LCSH search | Wikipedia search | 
|---|---|---|---|---|---|---|---|
| 1 | INTERNAL TIDES | 78 | 52% | 4% | 106 | Search INTERNAL+TIDES | Search INTERNAL+TIDES | 
| 2 | INTERNAL WAVES | 46 | 25% | 7% | 160 | Search INTERNAL+WAVES | Search INTERNAL+WAVES | 
| 3 | DIAPYCNAL MIXING | 18 | 48% | 1% | 27 | Search DIAPYCNAL+MIXING | Search DIAPYCNAL+MIXING | 
| 4 | PARAMETRIC SUBHARMONIC INSTABILITY | 14 | 100% | 0% | 7 | Search PARAMETRIC+SUBHARMONIC+INSTABILITY | Search PARAMETRIC+SUBHARMONIC+INSTABILITY | 
| 5 | BAROCLINIC TIDES | 9 | 67% | 0% | 8 | Search BAROCLINIC+TIDES | Search BAROCLINIC+TIDES | 
| 6 | NEAR INERTIAL WAVES | 8 | 70% | 0% | 7 | Search NEAR+INERTIAL+WAVES | Search NEAR+INERTIAL+WAVES | 
| 7 | STRATIFIED TURBULENCE | 8 | 30% | 1% | 23 | Search STRATIFIED+TURBULENCE | Search STRATIFIED+TURBULENCE | 
| 8 | INTERNAL WAVE BREAKING | 6 | 71% | 0% | 5 | Search INTERNAL+WAVE+BREAKING | Search INTERNAL+WAVE+BREAKING | 
| 9 | NEAR INERTIAL CURRENTS | 6 | 71% | 0% | 5 | Search NEAR+INERTIAL+CURRENTS | Search NEAR+INERTIAL+CURRENTS | 
| 10 | NEAR INERTIAL MOTIONS | 6 | 100% | 0% | 4 | Search NEAR+INERTIAL+MOTIONS | Search NEAR+INERTIAL+MOTIONS | 
| Key Words Plus | 
| Rank | Web of Science journal category | Relevance score (tfidf) | Class's shr. of term's tot. occurrences | Shr. of publ. in class containing term | Num. of publ. in class | 
|---|---|---|---|---|---|
| 1 | HAWAIIAN RIDGE | 236 | 88% | 5% | 113 | 
| 2 | ROUGH TOPOGRAPHY | 155 | 89% | 3% | 71 | 
| 3 | TURBULENT DISSIPATION | 146 | 72% | 5% | 115 | 
| 4 | KAENA RIDGE | 130 | 97% | 2% | 36 | 
| 5 | SURFACE MANIFESTATION | 114 | 93% | 2% | 42 | 
| 6 | ABYSSAL OCEAN | 103 | 56% | 5% | 124 | 
| 7 | BAROCLINIC TIDES | 89 | 79% | 2% | 57 | 
| 8 | INTERNAL WAVES | 72 | 24% | 11% | 269 | 
| 9 | DEEP OCEAN | 66 | 25% | 10% | 229 | 
| 10 | TIDAL ENERGY | 56 | 71% | 2% | 45 | 
| Journals | 
| Reviews | 
| Title | Publ. year | Cit. | Active references | % act. ref. to same field | 
|---|---|---|---|---|
| Internal tide generation in the deep ocean | 2007 | 187 | 67 | 70% | 
| Density stratification, turbulence, but how much mixing? | 2008 | 106 | 31 | 87% | 
| Vertical mixing, energy and thegeneral circulation of the oceans | 2004 | 481 | 80 | 50% | 
| Ocean Circulation Kinetic Energy: Reservoirs, Sources, and Sinks | 2009 | 114 | 104 | 49% | 
| Mixing efficiency in stratified shear flows | 2003 | 129 | 43 | 60% | 
| DIAPYCNAL MIXING IN THE THERMOCLINE - A REVIEW | 1987 | 442 | 55 | 82% | 
| TOWARD REGIONAL CHARACTERIZATIONS OF THE OCEANIC INTERNAL WAVEFIELD | 2011 | 18 | 114 | 75% | 
| Horizontal advection and dispersion in a stratified shelf sea: The role of inertial oscillations | 2013 | 4 | 11 | 64% | 
| The physical oceanography of Jones Bank: A mixing hotspot in the Celtic Sea | 2013 | 6 | 42 | 50% | 
| Internal gravity waves: From instabilities to turbulence | 2002 | 115 | 90 | 47% | 
| Address terms | 
| Rank | Address term | Relevance score (tfidf) | Class's shr. of term's tot. occurrences | Shr. of publ. in class containing term | Num. of publ. in class | 
|---|---|---|---|---|---|
| 1 | ENVIRONM FLUID DYNAM PROGRAM | 3 | 17% | 0.7% | 16 | 
| 2 | COBIA | 3 | 60% | 0.1% | 3 | 
| 3 | ENVIRONM FLUID MECH | 2 | 10% | 0.9% | 22 | 
| 4 | GEOG OCEANOG | 2 | 19% | 0.5% | 11 | 
| 5 | MARINE OBSERVAT | 2 | 67% | 0.1% | 2 | 
| 6 | PROGRAM ATMOSPHERE OCEAN SCI | 2 | 27% | 0.3% | 6 | 
| 7 | OCEAN FISHERY SCI OCEANOG | 1 | 100% | 0.1% | 2 | 
| 8 | RSCAMM SUPPORT PL MATH MODELING | 1 | 100% | 0.1% | 2 | 
| 9 | SCRIPPS OCEANOG MECH AEROSP ENGN | 1 | 50% | 0.1% | 2 | 
| 10 | OCEAN MODELLING FORECASTING GRP | 1 | 33% | 0.1% | 2 | 
| Related classes at same level (level 1) | 
| Rank | Relatedness score | Related classes | 
|---|---|---|
| 1 | 0.0000266588 | INTERNAL SOLITARY WAVES//INTERNAL SOLITARY WAVE//INTERNAL WAVES | 
| 2 | 0.0000192342 | STRATIFIED TURBULENCE//STRATIFIED FLUID//OSCILLATIONS OF A CYLINDER | 
| 3 | 0.0000168474 | OSCILLATING GRID TURBULENCE//SALINE WEDGE//TURBULENT ENTRAINMENT | 
| 4 | 0.0000151675 | SALT FINGERS//MAT SYST ENGN PL LIFE SCI//DOUBLE DIFFUSION | 
| 5 | 0.0000136840 | LANGMUIR CIRCULATION//STOKES DRIFT//WAVE INDUCED MIXING | 
| 6 | 0.0000120956 | SUBMESOSCALE//CYCLONIC EDDIES//MULTISCALE WINDOW TRANSFORM | 
| 7 | 0.0000112216 | TROPICAL CYCLONE HEAT POTENTIAL//UPPER OCEAN RESPONSE//SST COOLING | 
| 8 | 0.0000098427 | LAKE CIRCULATION//INTERNAL SEICHES//FREE SURFACE CORRECTION METHOD | 
| 9 | 0.0000095822 | STRAIT OF GIBRALTAR//HYDRAULIC CONTROL//OCEAN MODELLING UNIT | 
| 10 | 0.0000091610 | MARINE EXPEDIT//MATCHED FIELD METHOD//PELAGIC OOZE |