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Northwest Greenland experienced record melt, setting summer records for surface temperatures, production of meltwater, and total runoff.
Thermochemical properties of these specimens are given for surface temperatures between 1000 and 2000 K in pure oxygen and pure nitrogen plasmas.
The experiments and the modeling showed that methane was not an effective auxiliary fuel for surface temperatures up to about 1200 K.
Among-lake coherence was strong for surface temperatures and weak for the timing of stratification, suggesting individual lake characteristics mediate some – but not all – ecologically relevant lake responses to climate.
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Twelve K-type thermocouples for surface temperature measurements were installed in the grooves.
Information about the spatial distribution of urban surface emissivity is essential for surface temperature estimation.
Thermochromic Liquid Crystal (TLC) sheets were used for surface temperature measurements.
Only homogeneous spruce forest stands were used for surface temperature modeling.
The aim was to design a method for surface temperature normalisation of forest stands in rugged relief.
This work focuses on the design and characterization of polymer-encapsulated thermographic phosphor flexible sensors for surface temperature assessment.
In this work a method for surface temperature measurement based on contact sensors is presented.
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