You can
return it to the heat source to help it melt, but if you stir enough, it should melt on its own.
Not exact matches
Once it has passed over
heat exchangers, the warmed water will be
returned to the aquifer slightly downstream of the original
source.
So even though males will often move out
to search for new food
sources, a cat in
heat will certainly cause them
to return, or attract new males.
There could still be regional cooling in places like in the north Atlantic, which could slowdown melting on Greenland, and give the world an opportunity
to take advantage by putting the reduction of GHGs on the front burner asap
to mitigate the effects of albedo reduction and sea level rise from that
source, when the
heat returns.
The near - linear rate of anthropogenic warming (predominantly from anthropogenic greenhouse gases) is shown in
sources such as: «Deducing Multidecadal Anthropogenic Global Warming Trends Using Multiple Regression Analysis» «The global warming hiatus — a natural product of interactions of a secular warming trend and a multi-decadal oscillation» «The Origin and Limits of the Near Proportionality between Climate Warming and Cumulative CO2 Emissions» «Sensitivity of climate
to cumulative carbon emissions due
to compensation of ocean
heat and carbon uptake» «
Return periods of global climate fluctuations and the pause» «Using data
to attribute episodes of warming and cooling in instrumental records» «The proportionality of global warming
to cumulative carbon emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions
to ocean mixing»