Faktor vpliva za serijsko publikacijo Journal of Mountain Science za leto 2022
Leto
|
2022
|
Naslov serijske publikacije
|
Journal of Mountain Science
|
ISSN
|
1672-6316/1993-0321
|
Faktor vpliva
|
0.914
|
Uvrstitve Science Edition (SE) |
1904
|
2309
|
2306
|
1907
|
Earth-Surface Processes
|
Nature and Landscape Conservation
|
Global and Planetary Change
|
Geology
|
Uvrstitev
|
59/163
|
61/195
|
63/109
|
90/283
|
Četrtina
|
2
|
2
|
3
|
2
|
IFx
|
0.820
|
0.841
|
1.110
|
0.757
|
IFmax 1. četrtine
|
6.954
|
6.954
|
5.788
|
3.527
|
IFmin 1. četrtine
|
1.077
|
1.057
|
1.415
|
1.034
|
IFmax 2. četrtine
|
1.073
|
1.018
|
1.385
|
1.019
|
IFmin 2. četrtine
|
0.674
|
0.669
|
1.036
|
0.648
|
IFmax 3. četrtine
|
0.670
|
0.665
|
1.027
|
0.643
|
IFmin 3. četrtine
|
0.377
|
0.376
|
0.549
|
0.368
|
IFmax 4. četrtine
|
0.370
|
0.375
|
0.532
|
0.359
|
IFmin 4. četrtine
|
0.006
|
0.003
|
0.047
|
0.012
|
Uvrstitve Social Science Edition (SSE) |
3305
|
Geography, Planning and Development
|
Uvrstitev
|
306/759
|
Četrtina
|
2
|
IFx
|
0.929
|
IFmax 1. četrtine
|
16.903
|
IFmin 1. četrtine
|
1.220
|
IFmax 2. četrtine
|
1.219
|
IFmin 2. četrtine
|
0.736
|
IFmax 3. četrtine
|
0.735
|
IFmin 3. četrtine
|
0.427
|
IFmax 4. četrtine
|
0.425
|
IFmin 4. četrtine
|
0.003
|
ID=438631 Kreiran 05.10.2023 SNIP::IZUM |
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100 | | | a2022cJournal of Mountain Scienceh4980i249j0.914 |
110 | | | f1672-6316 |
120 | | | f1672-6316 |
200 | | | e1672-6316 |
210 | | | a1993-0321 |
300 | | | c1904dEarth-Surface Processesu59/163x0.820y0.674z1.0730216.95421.07731.07340.67450.67060.37770.37080.006 |
300 | | | c2309dNature and Landscape Conservationu61/195x0.841y0.669z1.0180216.95421.05731.01840.66950.66560.37670.37580.003 |
300 | | | c2306dGlobal and Planetary Changeu63/109x1.110y0.549z1.0270315.78821.41531.38541.03651.02760.54970.53280.047 |
300 | | | c1907dGeologyu90/283x0.757y0.648z1.0190213.52721.03431.01940.64850.64360.36870.35980.012 |
400 | | | c3305dGeography, Planning and Developmentu306/759x0.929y0.736z1.21902116.90321.22031.21940.73650.73560.42770.42580.003 |