File:Df_climate.png · Wikimedia Commons · See Wikimedia Commons
continental climate
Sign in to saveAlso known as Koppen D, D
main climate class in the Köppen climate classification system
A continental climate is one of the main climate types used by scientists to categorize and compare climates around the world. It matters because understanding climate classifications helps us predict weather patterns, plan for agriculture and infrastructure, and study how climates differ across regions.
AI-generated from the Wikipedia summary — may contain errors.
~8 min read
Encyclopedic overview
Areas of the world that feature a continental climate, according to Köppen
Continental climates in the Köppen climate classification often have a significant annual variation in temperature (warm to hot summers and cold winters). They tend to occur in central and eastern parts of the three northern-tier continents (North America and Eurasia), typically in the middle latitudes (40 to 55 or 60°N) , often within large landmasses, where prevailing winds blow overland bringing some precipitation, and temperatures are not moderated by oceans.
Excerpted from Wikipedia’s “continental climate” article, available under the CC BY-SA 4.0 licence.
Gallery (4)
Available in 66 languages
- Español
- Français
- Deutsch
- 中文
- 日本語
- Русский
- Português
- Italiano
- العربية
- हिन्दी
- Albanian
- Armenian
- Asturian
- Bahasa Indonesia
- Basque
- be_x_old
- Belarusian
- Bosnian
Show 47 more
- Bulgarian
- Catalan
- Cebuano
- Croatian
- Czech
- Danish
- Esperanto
- Estonian
- Finnish
- Galician
- Georgian
- Greek
- Hungarian
- Icelandic
- Kabyle
- Kannada
- Kazakh
- Latin
- Latvian
- Lithuanian
- Macedonian
- Malagasy
- Malay
- Nederlands
- Northern Frisian
- Norwegian
- Norwegian Nynorsk
- Occitan
- Polski
- Romanian
- Scots
- Serbian
- Serbian (Latin)
- simple
- Sinhala
- Slovak
- Svenska
- Tajik
- Tiếng Việt
- Türkçe
- Ukrainian
- Uzbek
- Western Frisian
- Wu Chinese
- zh_yue
- فارسی
- 한국어
via Wikidata sitelinks · CC0