Crkvice
Crkvice (Serbian/Montenegrin Cyrillic: Црквице, pronounced [t͡sř̩kv̞it͡sɛ]) is a village (42.34N 18.38E) on Orjen mountain in Montenegro and is the wettest inhabited place in Europe (although uninhabited locations such as Mýrdalsjökull in Iceland may receive significantly more precipitation[1]). The average annual precipitation for the period 1931-1960 was 4927 mm (l/m²) and for 1961-1990 4631 mm. The highest amounts per year surpass 7000 mm with an all time historic high at 8036 mm (1937).
Climate
Crkvice is within the Mediterranean subtropical belt. While summers are hot and sunny, autumn, winter and spring are rainy seasons. A peculiarity of the littoral Dinarids is the precipitation regime as the cities in Orjen receive more precipitation than any others in Europe. Like the monsoon rain it is seasonally distributed, thus November thunderstorms sometimes pour 2000 liters of water in several days, while August is frequently completely dry leading to forest fires. With a maximum discharge of 350 m³/s water one of the biggest karst springs, the Sopot spring, is a remarkable indicator of this seasonality. Most of the time it is inactive but after heavy rain a remarkable waterfall appears 20 m above the Bay of Kotor.
Station | Height [m] | Type | Character | Precipitation [mm] | Snow |
---|---|---|---|---|---|
Zubački kabao | 1894 | Dfsc | perhumid Mediterranean snowclimate | ca. 6250 | ap. 140 days |
Crkvice | 940 | Cfsb | (fs= without summerdryness), perhumid Mediterranean mountain climate | 4926 | 70 days |
Risan | 0 | Cs’’a | (s’’= double winter rain season), perhumid Mediterranean coast climate | 3500 | 2 days |
* classification scheme after Köppen
Two wind systems are noteworthy for their ecological significance: Bura and Jugo. Strong cold downslope winds of Bura type appear in winter and are most severe in the Bay of Risan. Gusts reach 250 km/h and can lead to a significant fall of temperatures in several hours with freezing events problematic for most of the Mediterranean cultures. Bura weather situations are frequent and sailors keep an eye on the mountains as cap clouds indicate an eminent Bura event. Jugo is a warm humid rain and is important as it brings heavy rain. It appears throughout the year but is usually centered in autumn and spring.
Station | Period | Height [m] | I | II | III | IV | V | VI | VII | VIII | IX | X | XI | XII | I-XII [mm/a] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Herceg Novi | 1961-1984 | 40 | 230 | 221 | 183 | 135 | 130 | 73 | 28 | 45 | 160 | 181 | 326 | 262 | 1974 |
Risan | 1961-1984 | 40 | 405 | 342 | 340 | 235 | 153 | 101 | 66 | 123 | 188 | 295 | 423 | 434 | 3105 |
Grahovo | 1961-1984 | 710 | 351 | 324 | 305 | 251 | 142 | 94 | 55 | 103 | 202 | 416 | 508 | 473 | 3224 |
Podvrsnik | 1961-1984 | 630 | 407 | 398 | 367 | 305 | 151 | 101 | 77 | 132 | 238 | 465 | 593 | 586 | 3820 |
Vrbanj | 1961-1984 | 1010 | 472 | 390 | 388 | 321 | 181 | 104 | 70 | 122 | 224 | 369 | 565 | 536 | 3742 |
Knezlaz | 1961-1984 | 620 | 547 | 472 | 473 | 373 | 207 | 120 | 72 | 136 | 268 | 400 | 629 | 661 | 4358 |
Crkvice | 1961-1984 | 940 | 610 | 499 | 503 | 398 | 198 | 135 | 82 | 155 | 295 | 502 | 714 | 683 | 4774 |
Ivan. Korita | 1960-1984 | 1350 | 434 | 460 | 742 | 472 | 128 | 198 | 74 | 46 | 94 | 300 | 694 | 972 | 4614 |
Goli vrh | 1893-1913 | 1311 | 271 | 286 | 307 | 226 | 188 | 148 | 75 | 70 | 215 | 473 | 415 | 327 | 3129 |
Jankov vrh | 1890-1909 | 1017 | 424 | 386 | 389 | 346 | 212 | 124 | 55 | 58 | 202 | 484 | 579 | 501 | 3750 |
Cetinje | 1961-1984 | 655 | 434 | 357 | 367 | 288 | 164 | 92 | 72 | 118 | 209 | 306 | 489 | 498 | 3394 |
Grab-Zubci | 1934-1960 | 677 | 333 | 325 | 257 | 195 | 183 | 83 | 59 | 86 | 173 | 360 | 447 | 485 | 2985 |
Trebinje | 1931-1960 | 276 | 193 | 190 | 160 | 102 | 119 | 70 | 43 | 76 | 110 | 239 | 247 | 249 | 1762 |
Dubrovnik | 1931-1960 | 49 | 147 | 113 | 102 | 92 | 79 | 60 | 24 | 38 | 97 | 156 | 213 | 186 | 1307 |
* monthly and yearly precipitation ranges in Dalmatia, Herzegovina and Montenegro
See also
References
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