Deep lakes warm very slowly in the spring, and small changes in water temperature at the end of winter can lead to large changes in the timing of summer stratification for these lakes.
Not exact matches
In response, lakebed temperatures of Arctic
lakes less than 1 meter (3 feet)
deep have
warmed by 2.4 degrees Celsius (4.3 degrees Fahrenheit) during the past three decades, and during five of the last seven years, the mean annual lakebed temperature has been above freezing.
In contrast, shallow
lakes warm much more quickly in the spring, so the timing of their summer stratification is much less variable than for
deep lakes.
Located along the Andes Mountains, it is the largest
lake in South America and is situated in such a way that mountain breezes tangle with
warm lake air to create a perfect storm, so to speak, of storms — an enduring
deep convection that results in 297 thunderstorms a year.
The invasion of Bythotrephes into
lakes in the northern US and Canada is unrelated to climate change, but is closely tied to the presence of a
deep water, low light relative
warm refuge from predatory fish.
However, there is no evidence at all for geothermal (volcanic
warming) of the
deeper waters of the
lake.
In addition, there are a completely unknown number of thermal vents directly
warming the bottoms of the oceans, and some
lakes, emitting a completely unknown amount of heat into the
deep water.