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Kuzmina, S. I., Johannessen, O. M., Bengtsson, L., Aniskina, O. G. & Bobylev, L. P. High northern latitude surface air temperature: comparison of existing data and creation of a new gridded data set 1900 2000.
The models developed for this study were able to estimate PAR for a given day, latitude, surface and atmospheric conditions using MATLAB.
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Changes in high-latitude surface temperatures and in southern hemisphere rainfall have also been attributed to the ozone loss24,25.
The latitudinal zones beyond 50 °N and 50 °S and three winter months (DJF) are excluded because polar amplification and albedo feedbacks dominate the high-latitude surface warming5,6.
The latitudinal zones beyond 50°N and 50°S and three winter months (DJF) are excluded because polar amplification and albedo feedbacks dominate the high-latitude surface warming5,6.
They added in a middle-of-the-road climate change scenario that caused high-latitude surface soil to rise 8 degrees Celsius by 2100, which is much greater than the global average.
In NH mid-latitudes, surface CH2Cl2 increases at a rate of 2.85 p.p.t. per year under Scenario 1 (Fig. 1c).
& Howat, I. M. Automated stereo-photogrammetric DEM generation at high latitudes: Surface Extraction with TIN-based Search-space Minimization (SETSM) validation and demonstration over glaciated regions.
Understanding this linkage is crucial to efforts aimed at predicting the consequences of the warming and freshening of high-latitude surface waters to the climate system.
The symmetric part of geomagnetic disturbance on the low-latitude surface is tracked and quantified by the disturbance storm time (Dst) index (Sugiura 1964) derived from variations of the horizontal components of geomagnetic observations at four low-latitude geomagnetic observatories (Sugiura and Kamei 1991).
Based on the spherical harmonic expansion of geomagnetic disturbance observed on the mid-latitude surface of the Earth, external and internal field separation is conducted in which the external component is magnetic disturbance caused by the magnetospheric ring current and the internal component is that raised by the correspondingly induced currents within the Earth.
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