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Gleisner, H., Thejll, P., Christianson, B. & Nielsen, J. K. Recent global warming hiatus dominated by low-latitude temperature trends in surface and troposphere data.
Further research is required to differentiate the individual contributions of these components on the observed trends in surface and upper tropospheric temperatures over land.
Further, binary mixtures of the model compounds were studied and found to produce unanticipated trends in surface charge density.
Multi-phase and multi component coating development is one of the present research trends in surface engineering arena.
Here we identify statistically significant trends in the occurrence of atmospheric circulation patterns, which partially explain observed trends in surface temperature extremes over seven mid-latitude regions of the Northern Hemisphere.
Periodic trends in the calculated potentials are found to be related to trends in surface segregation energies of the various solute/host pairs.
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We produced two key spatiotemporal datasets spanning the Arctic Coastal Plain of northern Alaska (~60,000 km2) to evaluate climate-geomorphological controls on arctic tundra productivity change, using (1) a novel 30 m classification of polygonal tundra geomorphology and (2) decadal-trends in surface greenness using the Landsat archive (1999 2014).
This trend is expected to reflect the trend in surface concentration of reactive amine groups as a function of bulk atomic nitrogen content.
In the present study, a corresponding trend in surface runoff DOC and river DOC indicates the role of hydrological factors influencing DOC production and export.
The long-term, linear, increasing trend in surface temperature [16] was removed before time-frequency analysis.
Although CCSM suggests a trend in surface air temperature of −0.012 °C/century under current conditions, −0.007 °C/century at 6,000 yBP, and −0.010 °C/century at 21,000 yBP, MIROC suggests 6e−04 °C/century under current conditions, −0.022 °C/century at 6,000 yBP, and −0.050 °C/century at 21,000 yBP.
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