Class information for: |
Basic class information |
Class id | #P | Avg. number of references |
Database coverage of references |
---|---|---|---|
2250 | 2307 | 42.5 | 58% |
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 |
147 | 3 | WATER RESOURCES//JOURNAL OF HYDROLOGY//SOIL EROSION | 63829 |
330 | 2 | WATER RESOURCES//JOURNAL OF HYDROLOGY//JOURNAL OF HYDROLOGIC ENGINEERING | 18102 |
2250 | 1 | RAINFALL RUNOFF MODEL//UNGAUGED CATCHMENTS//RAINFALL RUNOFF MODELLING | 2307 |
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 | RAINFALL RUNOFF MODEL | authKW | 560208 | 6% | 33% | 129 |
2 | UNGAUGED CATCHMENTS | authKW | 278447 | 2% | 48% | 44 |
3 | RAINFALL RUNOFF MODELLING | authKW | 224994 | 2% | 33% | 52 |
4 | WATER RESOURCES | WoSSC | 209640 | 80% | 1% | 1850 |
5 | JOURNAL OF HYDROLOGY | journal | 177312 | 17% | 3% | 399 |
6 | HYDROLOGICAL MODEL | authKW | 163396 | 3% | 17% | 71 |
7 | HYDROLOGY AND EARTH SYSTEM SCIENCES | journal | 156308 | 8% | 6% | 192 |
8 | PREDICTIONS IN UNGAUGED BASINS | authKW | 152577 | 1% | 82% | 14 |
9 | GLUE | authKW | 150835 | 3% | 18% | 63 |
10 | XINANJIANG MODEL | authKW | 132620 | 1% | 48% | 21 |
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 | Water Resources | 209640 | 80% | 1% | 1850 |
2 | Limnology | 31878 | 14% | 1% | 330 |
3 | Engineering, Civil | 25835 | 29% | 0% | 675 |
4 | Geosciences, Multidisciplinary | 16398 | 31% | 0% | 723 |
5 | Environmental Sciences | 9657 | 32% | 0% | 735 |
6 | Engineering, Environmental | 3785 | 11% | 0% | 246 |
7 | Computer Science, Interdisciplinary Applications | 1178 | 7% | 0% | 154 |
8 | Meteorology & Atmospheric Sciences | 530 | 5% | 0% | 114 |
9 | Agricultural Engineering | 89 | 1% | 0% | 22 |
10 | Statistics & Probability | 66 | 2% | 0% | 43 |
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 | WATER OURCES SECT | 80685 | 2% | 14% | 43 |
2 | HYDROL WATER OURCES | 69117 | 4% | 5% | 96 |
3 | OFF HYDROL DEV | 63385 | 1% | 22% | 22 |
4 | DIPARTIMENTO INGN IDRAUL PLICAZ AMBIENTALI | 62248 | 1% | 24% | 20 |
5 | INTEGRATED CATCHMENT ASSESSMENT MANAGEMENT | 59828 | 1% | 21% | 22 |
6 | HYDROSYST UNIT | 52937 | 0% | 100% | 4 |
7 | HYDROSYST BIOPROC UNIT HBAN | 49814 | 0% | 47% | 8 |
8 | HYDROL WATER QUAL UNIT | 42348 | 0% | 80% | 4 |
9 | CIVILIAN NUCL PROGRAM OFF SPO CNP | 39702 | 0% | 100% | 3 |
10 | WATER ECOSYST MANAGEMENT | 39702 | 0% | 100% | 3 |
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 HYDROLOGY | 177312 | 17% | 3% | 399 |
2 | HYDROLOGY AND EARTH SYSTEM SCIENCES | 156308 | 8% | 6% | 192 |
3 | WATER RESOURCES RESEARCH | 103155 | 14% | 3% | 313 |
4 | HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES | 81598 | 5% | 5% | 120 |
5 | HYDROLOGICAL PROCESSES | 60357 | 7% | 3% | 165 |
6 | HYDROLOGY RESEARCH | 49181 | 2% | 8% | 45 |
7 | JOURNAL OF HYDROLOGIC ENGINEERING | 40433 | 3% | 4% | 78 |
8 | ENVIRONMENTAL MODELLING & SOFTWARE | 35327 | 4% | 3% | 87 |
9 | JOURNAL OF HYDROINFORMATICS | 20001 | 1% | 5% | 31 |
10 | ADVANCES IN WATER RESOURCES | 17925 | 3% | 2% | 62 |
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 | RAINFALL RUNOFF MODEL | 560208 | 6% | 33% | 129 | Search RAINFALL+RUNOFF+MODEL | Search RAINFALL+RUNOFF+MODEL |
2 | UNGAUGED CATCHMENTS | 278447 | 2% | 48% | 44 | Search UNGAUGED+CATCHMENTS | Search UNGAUGED+CATCHMENTS |
3 | RAINFALL RUNOFF MODELLING | 224994 | 2% | 33% | 52 | Search RAINFALL+RUNOFF+MODELLING | Search RAINFALL+RUNOFF+MODELLING |
4 | HYDROLOGICAL MODEL | 163396 | 3% | 17% | 71 | Search HYDROLOGICAL+MODEL | Search HYDROLOGICAL+MODEL |
5 | PREDICTIONS IN UNGAUGED BASINS | 152577 | 1% | 82% | 14 | Search PREDICTIONS+IN+UNGAUGED+BASINS | Search PREDICTIONS+IN+UNGAUGED+BASINS |
6 | GLUE | 150835 | 3% | 18% | 63 | Search GLUE | Search GLUE |
7 | XINANJIANG MODEL | 132620 | 1% | 48% | 21 | Search XINANJIANG+MODEL | Search XINANJIANG+MODEL |
8 | HYDROLOGICAL MODELLING | 126967 | 3% | 15% | 65 | Search HYDROLOGICAL+MODELLING | Search HYDROLOGICAL+MODELLING |
9 | RAINFALL RUNOFF | 125545 | 2% | 19% | 51 | Search RAINFALL+RUNOFF | Search RAINFALL+RUNOFF |
10 | CONCEPTUAL RAINFALL RUNOFF MODELS | 112094 | 1% | 71% | 12 | Search CONCEPTUAL+RAINFALL+RUNOFF+MODELS | Search CONCEPTUAL+RAINFALL+RUNOFF+MODELS |
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 | HRACHOWITZ, M , SAVENIJE, HHG , BLOSCHL, G , MCDONNELL, JJ , SIVAPALAN, M , POMEROY, JW , ARHEIMER, B , BLUME, T , CLARK, MP , EHRET, U , ET AL (2013) A DECADE OF PREDICTIONS IN UNGAUGED BASINS (PUB)A REVIEW.HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES. VOL. 58. ISSUE 6. P. 1198 -1255 | 189 | 32% | 152 |
2 | EFSTRATIADIS, A , KOUTSOYIANNIS, D , (2010) ONE DECADE OF MULTI-OBJECTIVE CALIBRATION APPROACHES IN HYDROLOGICAL MODELLING: A REVIEW.HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES. VOL. 55. ISSUE 1. P. 58-78 | 72 | 79% | 115 |
3 | SADEGH, M , VRUGT, JA , (2013) BRIDGING THE GAP BETWEEN GLUE AND FORMAL STATISTICAL APPROACHES: APPROXIMATE BAYESIAN COMPUTATION.HYDROLOGY AND EARTH SYSTEM SCIENCES. VOL. 17. ISSUE 12. P. 4831 -4850 | 81 | 74% | 5 |
4 | VRUGT, JA , TER BRAAK, CJF , DIKS, CGH , SCHOUPS, G , (2013) HYDROLOGIC DATA ASSIMILATION USING PARTICLE MARKOV CHAIN MONTE CARLO SIMULATION: THEORY, CONCEPTS AND APPLICATIONS.ADVANCES IN WATER RESOURCES. VOL. 51. ISSUE . P. 457 -478 | 70 | 69% | 46 |
5 | HRACHOWITZ, M , FOVET, O , RUIZ, L , EUSER, T , GHARARI, S , NIJZINK, R , FREER, J , SAVENIJE, HHG , GASCUEL-ODOUX, C , (2014) PROCESS CONSISTENCY IN MODELS: THE IMPORTANCE OF SYSTEM SIGNATURES, EXPERT KNOWLEDGE, AND PROCESS COMPLEXITY.WATER RESOURCES RESEARCH. VOL. 50. ISSUE 9. P. 7445 -7469 | 63 | 64% | 33 |
6 | BEVEN, K , BINLEY, A , (2014) GLUE: 20 YEARS ON.HYDROLOGICAL PROCESSES. VOL. 28. ISSUE 24. P. 5897 -5918 | 61 | 67% | 27 |
7 | HERMAN, JD , REED, PM , WAGENER, T , (2013) TIME-VARYING SENSITIVITY ANALYSIS CLARIFIES THE EFFECTS OF WATERSHED MODEL FORMULATION ON MODEL BEHAVIOR.WATER RESOURCES RESEARCH. VOL. 49. ISSUE 3. P. 1400-1414 | 56 | 79% | 28 |
8 | GUPTA, HV , PERRIN, C , BLOSCHL, G , MONTANARI, A , KUMAR, R , CLARK, M , ANDREASSIAN, V , (2014) LARGE-SAMPLE HYDROLOGY: A NEED TO BALANCE DEPTH WITH BREADTH.HYDROLOGY AND EARTH SYSTEM SCIENCES. VOL. 18. ISSUE 2. P. 463 -477 | 60 | 64% | 37 |
9 | GHARARI, S , HRACHOWITZ, M , FENICIA, F , GAO, H , SAVENIJE, HHG , (2014) USING EXPERT KNOWLEDGE TO INCREASE REALISM IN ENVIRONMENTAL SYSTEM MODELS CAN DRAMATICALLY REDUCE THE NEED FOR CALIBRATION.HYDROLOGY AND EARTH SYSTEM SCIENCES. VOL. 18. ISSUE 12. P. 4839 -4859 | 73 | 58% | 15 |
10 | SHAFII, M , TOLSON, BA , (2015) OPTIMIZING HYDROLOGICAL CONSISTENCY BY INCORPORATING HYDROLOGICAL SIGNATURES INTO MODEL CALIBRATION OBJECTIVES.WATER RESOURCES RESEARCH. VOL. 51. ISSUE 5. P. 3796 -3814 | 54 | 76% | 7 |
Classes with closest relation at Level 1 |