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  2. Lake Oswego - Wikipedia

    en.wikipedia.org/wiki/Lake_Oswego

    www.ci.oswego.or.us. Lake Oswego (/ ɒsˈwiːɡoʊ / oss-WEE-goh) is a city in the U.S. state of Oregon, primarily in Clackamas County, with small portions extending into neighboring Multnomah and Washington counties. [4] Population in 2020 was 40,731, an 11.2% increase since 2010, making it the 11th most populous city in Oregon.

  3. Lake-effect snow - Wikipedia

    en.wikipedia.org/wiki/Lake-effect_snow

    A cold northwesterly to westerly wind over all the Great Lakes created the lake-effect snowfall of January 10, 2022. Lake-effect snow is produced during cooler atmospheric conditions when a cold air mass moves across long expanses of warmer lake water. The lower layer of air, heated by the lake water, picks up water vapor from the lake and ...

  4. Past sea level - Wikipedia

    en.wikipedia.org/wiki/Past_sea_level

    Sea levels have been comparatively stable over the past 6,500 years, ending with a 0.50 m sea level rise over the past 1,500 years. For example, about 10,200 years ago the last land bridge between mainland Europe and Great Britain was submerged, leaving behind a salt marsh. By 8000 years ago the marshes were drowned by the sea, leaving no trace ...

  5. Oswego Lake - Wikipedia

    en.wikipedia.org/wiki/Oswego_Lake

    Oswego Lake is a lake in Clackamas County, Oregon, United States, that is completely surrounded by the city of Lake Oswego. Though the lake is naturally occurring (a former channel of the Tualatin River ), it has been significantly altered because of the concrete dam that has increased its size to 431.7 acres (1.747 km 2 ).

  6. Great Barrier Reef waters were hottest in 400 years over the ...

    www.aol.com/news/great-barrier-reef-waters-were...

    August 7, 2024 at 11:02 AM. WASHINGTON (AP) — Ocean temperatures in the Great Barrier Reef hit their highest level in 400 years over the past decade, according to researchers who warned that the ...

  7. Post-glacial rebound - Wikipedia

    en.wikipedia.org/wiki/Post-glacial_rebound

    Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression. Post-glacial rebound and isostatic depression are phases of glacial isostasy (glacial isostatic adjustment, glacioisostasy ...

  8. Effects of climate change on oceans - Wikipedia

    en.wikipedia.org/wiki/Effects_of_climate_change...

    Global map of low and declining oxygen levels in the open ocean and coastal waters. The map indicates coastal sites where anthropogenic nutrients have resulted in oxygen declines to less than 2 mg L –1 (red dots), as well as ocean oxygen minimum zones at 300 metres (blue shaded regions). [54]

  9. ‘The ocean is overflowing’: UN chief issues global ... - AOL

    www.aol.com/news/ocean-overflowing-un-chief...

    If the world continues its path of heating to 3 degrees Celsius above pre-industrial levels, the Pacific Islands can expect to see at least another 15 centimeters of additional sea level rise by ...