58th parallel north

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The 58th parallel north is a circle of latitude that is 58 degrees north of the Earth's equatorial plane. It crosses Europe, Asia, the Pacific Ocean, North America, and the Atlantic Ocean. At this latitude the Sun is visible for 18 hours, 11 minutes during the summer solstice and 6 hours, 27 minutes during the winter solstice.

Around the world

Starting at the Prime Meridian and heading eastwards, the parallel 58ยฐ north passes through: ! scope="col" width="125" | Coordinates ! scope="col" | Country, territory or ocean ! scope="col" | Notes ! scope="row" style="background:#b0e0e6;" | North Sea ! scope="row" | ๐Ÿ‡ณ๐Ÿ‡ด ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" | ๐Ÿ‡ณ๐Ÿ‡ด ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" style="background:#b0e0e6;" | Skagerrak Passing between Vรฅre Island to the north and Udvรฅre Island to the south, Vest-Agder ! scope="row" | ๐Ÿ‡ณ๐Ÿ‡ด ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" style="background:#b0e0e6;" | Skagerrak ! scope="row" | ๐Ÿ‡ณ๐Ÿ‡ด ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" style="background:#b0e0e6;" | Skagerrak Passing south of Uvรฅr and Songvรฅr Islands, Vest-Agder ! scope="row" | ๐Ÿ‡ธ๐Ÿ‡ช ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" style="background:#b0e0e6;" | Hakefjorden ! scope="row" | ๐Ÿ‡ธ๐Ÿ‡ช ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" | ๐Ÿ‡ช๐Ÿ‡ช ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" | ๐Ÿ‡ช๐Ÿ‡ช ! scope="row" | ๐Ÿ‡ฑ๐Ÿ‡ป ! scope="row" | ๐Ÿ‡ช๐Ÿ‡ช ! scope="row" | ๐Ÿ‡ฑ๐Ÿ‡ป ! scope="row" | ๐Ÿ‡ช๐Ÿ‡ช ! scope="row" | ๐Ÿ‡ท๐Ÿ‡บ ! scope="row" style="background:#b0e0e6;" | Pacific Ocean ! scope="row" | ๐Ÿ‡ท๐Ÿ‡บ ! scope="row" style="background:#b0e0e6;" | Pacific Ocean ! scope="row" | ๐Ÿ‡บ๐Ÿ‡ธ ! scope="row" style="background:#b0e0e6;" | Pacific Ocean ! scope="row" | ๐Ÿ‡บ๐Ÿ‡ธ ! scope="row" style="background:#b0e0e6;" | Pacific Ocean ! scope="row" | ๐Ÿ‡บ๐Ÿ‡ธ ! scope="row" | ๐Ÿ‡จ๐Ÿ‡ฆ ! scope="row" style="background:#b0e0e6;" | Arctic Ocean ! scope="row" | ๐Ÿ‡จ๐Ÿ‡ฆ ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" | ! scope="row" style="background:#b0e0e6;" | The Minch ! scope="row" | ! scope="row" style="background:#b0e0e6;" | North Sea

Climate

In general, this parallel sees significant differences in temperature and precipitation with proximity to warm ocean currents. The moderation from the Gulf Stream ensures a moderate oceanic climate in much of Western Europe and on the immediate coastline of Alaska, whereas moving inland on continental masses, subarctic climates predominate as the dark winters dominate the temperature cycle. In the transitional area centred on the Baltic Sea this latitude sees a humid continental climate with warm summers and snowy winters somewhat below freezing. Where cold ocean currents dominate such as near Hudson Bay the climate is polar, rendering in severe winter conditions and very subdued summers. This type of climate is seen in the surroundings of Inukjuak in Quebec, Canada, where the sea ice eliminates winter moderation, but the thawing of the cold water renders in very cool summers as well. In more continental cold areas such as these winters commonly go below -30 C even during the day. Further west in inland areas winters are often as severe, but summers average above 22 C, similar to the Baltic region where climates are much gentler.

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