Sauyin yanayi na Norway

**yanayin Norway** ya fi dacewa fiye da yadda ake tsammani don manyan latitudes. Wannan yafi yawa saboda Arewacin Atlantic Current tare da tsawo, Norwegian Current, yana haɓaka zafin iska;  yawancin kudu maso yammacin da ke kawo iska mai sauƙi a bakin teku; da kuma gabaɗaya kudu maso yamma-arewa maso gabas na bakin tekun, wanda ke ba da damar yammacin shiga cikin Arctic. Matsakaicin Janairu a Brønnøysund  shine  ° C (59 ° F) sama da matsakaicin Janairun a Nome, Alaska,  duk da cewa garuruwan biyu suna kan iyakar yammacin nahiyoyi a 65 ° N. A watan Yuli an rage bambancin zuwa  ° C (37.8 ° F). Matsakaicin watan Janairu na Yakutsk, a Siberia amma dan kadan a kudu, shine -42.3 ° C (−44.1 ° F) ƙasa da Brønnøysund . 

## Ruwan sama

Norway tana cikin ƙasashe mafi ƙasƙanci na Turai, amma tare da bambancin yawan hazo saboda yanayin ƙasa mai sarƙoƙin tsaunuka wanda ke haifar da hazo na orographic amma kuma yana haifar da inuwar ruwan sama.  A wasu yankuna, wurare masu yawan hazo daban-daban na iya zama kusa da juna.  Gundumar Stryn (1661 mm) tana samun hazo ninki 6 kamar yadda Skjåk ke tafiyar minti 90, Bergen yana da hazo ninki biyar fiye da gundumar Lærdal a yanki ɗaya, kuma a arewacin Glomfjord (2141 mm) ana samun hazo sau 10 fiye da ninki 10 na sama sama da 6 m Saltdal.  Wasu yankuna na Vestlandet da kudancin Nordland suna cikin mafi ƙanƙanta a Turai, saboda ɗagawa na orographic, musamman inda manyan tsaunuka suka fara kama yankunan yammaci.  Wannan yana faruwa kaɗan a cikin ƙasa daga waje mai gadin skerry.  A cikin sabuntar al'ada na 1991-2020, Gullfjellet a Bergen (345m) yana da hazo mafi girma na shekara tare da 4,067 mm (160.1 in).  Hazo na shekara na iya wuce 5,000 mm (196.9 in) a yankunan tsaunuka kusa da bakin teku.  Lurøy Municipality a Arctic Circle yana samun 3,066 mm (120.7 in) kowace shekara, adadi mai ban mamaki don wurin polar.  Hazo ya fi yin nauyi a ƙarshen kaka da hunturu a bakin tekun, yayin da Afrilu zuwa Yuni ya fi bushewa.  Sassan ciki na dogayen fjords sun ɗan bushewa: hazo shekara-shekara a gundumar Lærdal shine 514 mm (20.2 in), kuma a arewa kawai 338 mm (13.3 in) a Skibotn a shugaban Lyngenfjord.  Yankunan gabas na sarkar tsaunuka (ciki har da Oslo) suna da yanayi na nahiya da ke da ƙarancin hazo, da hazo kololuwa a lokacin rani da farkon kaka, yayin da hunturu da bazara sukan zama bushewa.  Babban yanki a cikin ƙasar Finnmark yana samun ƙasa da 450 mm (17.7 in) na hazo kowace shekara.  Wasu kwaruruka da ke kewaye da tsaunuka suna samun ƙarancin hazo, kuma galibi suna buƙatar ban ruwa a lokacin rani.  Babban yanki na gundumar Saltdal (m 81, Storjord) yana da matsakaicin matsakaicin shekara mafi ƙanƙanta da mm 211 kawai (8.3 in), yayin da a kudancin Norway, Skjåk ya fi bushewa da 295 mm (11.6 in).  A cikin manyan tsibirai na Arctic na Norway, Filin jirgin saman Svalbard yana da matsakaicin matsakaicin hazo na shekara tare da 217 mm (8.5 in), yayin da Jan Mayen ya sami fiye da ninki biyu da 648 mm (25.5 in).&nbsp;

Matsakaicin kowane wata ya bambanta daga   in)  Disamba a Gullfjellet. Yankunan bakin teku daga Lindesnes Municipality arewa zuwa Vardø Municipality suna da fiye da kwanaki 200 a kowace shekara tare da hazo; duk da haka, wannan yana da ƙarancin ƙimar ƙofar (0.1 mm hazo). Matsakaicin adadin kwanaki na shekara-shekara tare da akalla 3  in) hazo shine 77 a Blindern / Oslo, 96 a Kjevik / Christian, 158 a Florida / Bergen, 93 a Værnes / Trondheim, da 109 a Tromsø.&nbsp;

The coast experiences milder winters than other areas at the same latitudes. The average temperature difference between the coldest month and the warmest is only  in coastal areas; some lighthouses have a yearly amplitude of just , such as Svinøy in Herøy Municipality with a coldest month of . The differences of inland areas are larger, with a maximum difference of  in Karasjok Municipality. Finnmarksvidda has the coldest winters in mainland Norway, but inland areas much further south can also experience severe cold. Røros Municipality has recorded .

Karamar Hukumar Bø ita ce wurin da ta fi arewa a duniya inda duk watannin hunturu ke da ma'anar zafi sama da 0 °C (32 °F).  Lokacin bazara shine lokacin da bambance-bambancen yanayin zafi tsakanin kudanci da arewacin kasar ya fi girma;  wannan kuma lokaci ne na shekara da yanayin rana da dare suka fi bambanta.  Kwaruruka na cikin gida da wuraren fjord na ciki suna da ƙarancin iska kuma suna ganin kwanakin bazara mafi zafi.  Ƙasar ƙasa kusa da Oslo ita ce mafi zafi a lokacin rani tare da matsakaita 24 ga Yuli-hr na 18 °C (64.4 °F) da matsakaita yau da kullun har zuwa 23 °C (73.4 °F).  Yankunan cikin ƙasa suna samun zafi a tsakiyar watan Yuli da yankunan bakin teku a farkon rabin watan Agusta.  Yawan danshi ba ya da yawa a lokacin rani.

Yankin Arewacin Atlantic ya rabu kashi biyu a arewacin Tekun Norway, reshe daya yana zuwa gabas zuwa Tekun Barents ɗayan kuma yana zuwa arewa tare da gabar yammacin Spitsbergen. Wannan yana canza yanayin Arctic polar dan kadan kuma yana haifar da ruwa mai budewa a duk shekara a mafi girman latitudes fiye da kowane wuri a cikin Arctic. A gabar gabashin tsibirin Svalbard, teku ta kasance mai daskarewa a mafi yawan shekara, amma yanayin zafi na shekarun da suka gabata (graph) ya ga ruwa mai budewa ya fi tsayi.

Yawan zafin jiki mafi zafi da aka taɓa yin rikodin a Norway shine  ° C (96.1 ° F) a cikin Nesbyen Municipality. Yawan zafin jiki mafi sanyi shine -51.4   a Karasjok Municipality. Watan da ya fi zafi a rubuce shi ne Yuli  a Oslo, tare da matsakaicin zafin jiki na awa 24 na  ° C (72.9 ° F)), kuma watan da ya fi sanyi shi ne Fabrairu 1966 a Karasjok, tare da ma'auni na -27.1 ° C (-16.8 ° F). Dare mafi zafi da aka rubuta a Norway shine 29 ga Yuli, 2019 a Sømna-Kvaløyfjellet (302 m) a Sømn Municipalitya kusa da Brønnøysund tare da dare  ° C (79.0 ° F).  Rashin iska mai sauƙi a cikin hunturu wanda ya kara da zafi ta hanyar foehn na iya ba da yanayin zafi a cikin ƙananan fjords a cikin hunturi: Sunndalsøra ya rubuta 19 ° C (66 ° F) a cikin Janairu da  ° C (66.0 ° F) cikin Fabrairu.

Idan aka kwatanta da yankunan bakin teku, kwari na cikin gida da yankunan da ke cikin gida suna da bambancin zafin jiki na rana, musamman a lokacin bazara da rani.

## Hasken rana, yankunan lokaci, da raƙuman ruwa
Yankunan da ke Norway da ke arewacin Arctic Circle suna da matsanancin duhu a cikin hunturu, wanda ke ƙaruwa tare da latitude. A Longyearbyen a tsibirin Svalbard a cikin iyakar arewa, saman ɓangaren rana yana sama da sararin samaniya daga 9 ga Afrilu zuwa 23 ga Agusta, kuma duhu na hunturu yana daga 27 ga Oktoba zuwa 14 ga Fabrairu. Duhu na hunturu ba duhu ba ne a arewacin yankin, saboda akwai faɗuwar rana na 'yan sa'o'i a kusa da tsakar rana. 

Yankin kudancin kasar kuma yana fuskantar manyan bambance-bambance na yanayi a hasken rana; a Oslo, rana tana fitowa a 03:54 kuma tana saita 22:54 a lokacin rani, amma tana sama da sararin samaniya daga 09:18 zuwa 15:12 a lokacin hunturu. Yankin arewacin ƙasar yana cikin yankin aurora borealis; ana ganin aurora a wasu lokuta a kudancin ƙasar.

Norway tana kan Lokacin Tsakiyar Turai, daidai da 15°E longitude.  Da yake ƙasar tana da tsayi sosai, hakan ya yi hannun riga da sa'o'in hasken rana a yankunan gabashi da yamma.  A Vardø, lokacin hasken rana na gida yana da mintuna 64 da suka gabata, kuma a Bergen, mintuna 39 ne daga baya.  Don haka, Finnmark yana samun hasken safiya amma yana rasa hasken rana, kuma Vestlandet yana rasa hasken safiya amma yana samun ƙarin hasken rana a wannan yankin lokaci.  Ana lura da lokacin adana hasken rana (GMT + 2) daga Lahadi ta ƙarshe a cikin Maris zuwa Lahadi ta ƙarshe a cikin Oktoba.

Bambanci tsakanin low tide da high tide ne karami a kudancin gabar kuma babba a arewa; daga matsakaicin 0.17 m a Mandal zuwa game da 0.30 m a Oslo da Stavanger, 0.90 m a Bergen, 1.80 m a Trondheim, Bodø da Hammerfest kuma kusan 2.17 m a Vadsø.

## Misalan

### Tebur
} and  the climate zone is named as Cfb/Dfb (or Cfc/Dfc) as Europe and US use different winter thresholds between C/D climates. *Cfb*=temperate oceanic/marine west coast; *Dfb*=humid continental; *Cfc*=subpolar oceanic (cold oceanic); *Dfc*=boreal/subarctic; *ET*=polar tundra or alpine tundra. Sep and Nov used to illustrates different climate zones better. *Sognefjellhytta*: Mountain lodge along Sognefjellsvegen west of Jotunheimen.*Snow:* Number of days/year with at least  snow on the ground; 1971–2000 base period. Due to warming most lowland areas have less snow in recent years. Snow data from nearby: Rørvik for Brønnøysund, Karasjok for Kautokeino, Tromsø snow from 100 m ASL; Molde snow  1979 - 87. Some locations have Feb colder than Jan; some coastal stations have Aug warmer than Jul.
|}
Kamar ya*D* aka gani daga t*E*, yanayin Norway yana nuna bamban*C*-bambance masu yawa, amma duk yankunan da ke zaune a yankin Norway suna da yanayin yanayi ko yanayin subarctic (ƙungiyoyin Köppen C da D). Svalbard da Jan Mayen suna da yanayin polar (Köppen group E).

A sakamakon dumama tun 1990, lokacin rani yana da zafi kuma ya fi tsayi kuma hunturu yana raguwa da sauƙi. Tare da sabon yanayi na 1991-2020 na al'ada, yankuna da yawa sun ga canjin yanayi zuwa sabon yankin yanayi idan aka kwatanta da na 1961-90 na al'adu. Yanayin Oslo ya koma daga Dfb zuwa Cfb / DFb, Lillehammer daga Dfc zuwa Dfb, Kristiansand daga Cfb - DFb zuwa CFb, Molde da Brønnøysund daga Cfc / DFc zuwa Cfc, Trondheim daga Dffc zuwa CFc, Bodø daga Cf c / DFc to Cfb, Tromsø (Holt) daga Df c / Dfc Ruwan dusar ƙanƙara ya ragu a mafi yawan wuraren da ke da yawan jama'a saboda yanayin zafi na hunturu; kwanaki / shekara tare da murfin dusar ƙara na 25 cm a cikin 1991-2020 kwanaki 26 ne a Oslo (94 m), kwanaki 2 a Bergen, kwanaki 8 a Trondheim / Værnes da kwanaki 144 a Tromsø. An lura da zafi mafi karfi a Svalbard. Baya ga dumama, hazo ya karu a mafi yawan yankuna, musamman a cikin hunturu, karuwar rushewa da haɗarin rushewar ƙasa.&nbsp;

### akwatunan yanayi

## Canjin yanayi

## Manazarta