The scientists simulated
how lake temperatures would probably rise through the year 2089 and how that might affect walleye survival in the state's lakes.
Not exact matches
And at the University of Exeter in England,
lake expert Gabriel Yvon - Durocher has been working to measure, on a small scale,
how exactly ponds and
lakes will respond to rising
temperatures.
This is what I wrote on July 26th, 2007 about it in:
How Not to Measure
Temperature, Part 25 This picture, taken by www.surfacestations.org volunteer Don Kostuch is the Detroit
Lakes, MN USHCN climate -LSB-...]
Unfortunately, in their paper they neglected to show
how the
Lake Tanganyika LST «closely tracks air
temperatures over the instrumental period» of the «past half - century».
They do say they calibrate it against the
lake itself, but they give absolutely no indication as to what
temperature dataset they are using or
how they are doing the «calibration»... which makes me suspicious.
If we have virtually no data about the
lake surface
temperature,
how can we even estimate what the error of what is only an educated guess might be?
I am going to talk about
how changes with local
temperature, pikas, whitebark park pines, and snowpack, may be an indication global climate change is impacting Crater
Lake.»
Such «ice balls» have even formed on
lake water that was 40 degrees,
how is this possible at
temperatures far above the normal freezing point?
The profile also demonstrates
how temperatures can vary across a city depending on the nature of the land cover, such that urban parks and
lakes are cooler than adjacent areas covered by buildings.
Meanwhile, Ukstins Peate's team determines composition, mineral content, and
temperature information, showing
how the structure of the land around the
lake changed as
temperatures dropped.
The models (and there are many) have numerous common behaviours — they all cool following a big volcanic eruption, like that at Mount Pinatubo in 1991; they all warm as levels of greenhouse gases are increased; they show the same relationships connecting water vapour and
temperature that we see in observations; and they can quantify
how the giant
lakes left over from the Ice Age may have caused a rapid cooling across the North Atlantic as they drained and changed ocean circulation patterns.