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58th parallel north
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" | ๐ณ๐ด ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" | ๐ณ๐ด ! 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" | ๐ณ๐ด ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" style="background:#b0e0e6;" | Skagerrak ! scope="row" | ๐ณ๐ด ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" style="background:#b0e0e6;" | Skagerrak Passing south of Uvรฅr and Songvรฅr Islands, Vest-Agder ! scope="row" | ๐ธ๐ช ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" style="background:#b0e0e6;" | Hakefjorden ! scope="row" | ๐ธ๐ช ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" | ๐ช๐ช ! scope="row" style="background:#b0e0e6;" | Atlantic Ocean ! scope="row" | ๐ช๐ช ! scope="row" | ๐ฑ๐ป ! scope="row" | ๐ช๐ช ! scope="row" | ๐ฑ๐ป ! scope="row" | ๐ช๐ช ! scope="row" | ๐ท๐บ ! scope="row" style="background:#b0e0e6;" | Pacific Ocean ! scope="row" | ๐ท๐บ ! scope="row" style="background:#b0e0e6;" | Pacific Ocean ! scope="row" | ๐บ๐ธ ! scope="row" style="background:#b0e0e6;" | Pacific Ocean ! scope="row" | ๐บ๐ธ ! scope="row" style="background:#b0e0e6;" | Pacific Ocean ! scope="row" | ๐บ๐ธ ! scope="row" | ๐จ๐ฆ ! scope="row" style="background:#b0e0e6;" | Arctic Ocean ! scope="row" | ๐จ๐ฆ ! 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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