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The temperature of the eastern tropical Pacific fluctuates between relative warm (El Niño) and relatively cold (La Niña) every 2 to 8 years, based on well-known instrumental records from the recent past.
To infer possible future landscape changes in the McMurdo Dry Valleys, due to anticipated climate warming, we map 'at risk' landscapes defined as those with buried massive ice in relative warm regions of the valleys.
The great amount of precipitation and relative warm environments in summer suggests that soils might experience intense dry-wet processes, and this probably stimulated soil microbes to greatly utilise organic N resources in soils.
Behind extratropical cyclones, rainbands can form downwind of relative warm bodies of water such as the Great Lakes.
In addition, we found that foragers collected in the early fall (relative warm, long days) exhibit a delay in the nightly peak of period expression relative to foragers collected in the early spring (relative cold, short days).
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I don't think that much emphasis has been given to the difference in warming between the N.H. and S.H. "You seems to be suggesting that the relative warming of the N.H. is caused by ice loss, rather than the other way around". Ice and snow loss is one of the main feedback mechanisms for warming.
"This is consistent with the accelerated ice loss seen in the NH, which has reduced its albedo and increased its capacity to absorb solar energy". You seems to be suggesting that the relative warming of the N.H. is caused by ice loss, rather than the other way around.
Qualitative analyses, i.e., detection of relative warming and cooling, remain justified using physiognomic data from well-understood regional floras that have supporting data on taxonomy, paleogeography, and distribution of traits along independently inferred paleotemperature gradients (i.e. using floras from several latitudinally adjacent basins).
Urban location is considered a risk factor for vulnerability to climate stressors, due in part to the exacerbation of summer heat by the urban heat island effect (a term that describes the relative warming of urban areas compared with their rural surroundings due to the replacement of open land and vegetation with buildings, roads, and other dark or impermeable surfaces) (CCSP 2008).
Other studies of AFO waste have noted higher estrogen levels in cool months relative to warm months, with one study suggesting decreased photolysis and inhibition of bacteria-mediated degradation processes as a possible explanation for this trend.
Deangelis et al. (2015) reported that some members of the Actinobacteria, Alphaproteobacteria and Acidobacteria showed strong warming responses in temperate forest soils, with one Actinomycete decreasing from 4.5 to 1% relative to warming (5 °C increased).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com