Editing Subarctic climate (section)

===''Dsc'' and ''Dsd'' distribution===
Climates classified as ''Dsc'' or ''Dsd'', with a dry summer, are rare, occurring in very small areas at high elevation around the [[Mediterranean Basin]]; [[Iran]]; [[Kyrgyzstan]]; [[Tajikistan]]; [[Alaska]] and other parts of the [[northwestern United States]] ([[Eastern Washington]], [[Eastern Oregon]], [[Southern Idaho]], California's [[Eastern Sierra]]); the [[Russian Far East]]; [[Akureyri, Iceland]]; [[Seneca, Oregon]]; and [[Atlin, British Columbia]]. [[Turkey]] and [[Afghanistan]] are exceptions; ''Dsc'' climates are common in [[Northeast Anatolia Region (statistical)|Northeast Anatolia]], in the [[Taurus Mountains|Taurus]] and [[Köroğlu Mountains]], and the [[Central Afghan highlands]].

In the Southern Hemisphere, the Dsc climate is present in [[South America]] as a subarctic climate influenced by Mediterranean characteristics, often considered a high-altitude variant of the Mediterranean climate. It is located on the eastern slopes of the central Argentine [[Andes]] and in some sections on the Chilean side. While there are no major settlements exhibiting this climate, several localities in the vicinity experience it, such as [[San Carlos de Bariloche]], [[Villa La Angostura]], [[San Martín de los Andes]], [[Balmaceda, Chile|Balmaceda]], [[Punta de Vacas]], and [[Termas del Flaco]].<ref>{{cite web |last1=Sanchez Davila |first1=Gabriel |title=Clasificación climática de Sudamérica |url=https://storymaps.arcgis.com/stories/b74200791dda49958d6d39eddaca74a0/preview#n-KOOVnv |website=StoryMaps |publisher=ArcGIS |access-date=30 April 2024 |date=2021}}</ref>