HRES - O1280
- Temperature at 2m has been interpolated from the O1280 target grid to regular lat-lon grids at different resolutions
- Differences between MIR and EMOSLIB generally lie between +/-5K.
- In general, more than 95% of points differ by less than+/-1K.
- Largest differences occur close to the coasts and in areas of steep orography where the gradient of the 2m temperature field changes most rapidly
- The plots show the differences with the contours chosen on a logarithmic scale. Grid points where the absolute difference is greater than 50% of the maximum absolute difference are indicated with red (EMOSLIB greater than MIR) and blue (EMOSLIB less than MIR) filled circle
Target resolution | Statistics of differences | Histogram of differences | Global | Europe |
---|---|---|---|---|
0.1x0.1 | Maximum difference = 4.757812 | -4.757812 : -3.806250 - 2 (0.000031%) | ||
0.125x0.125 | Maximum difference = 5.131653 | -5.131653 : -4.105322 - 0 ( 0.000000%) | ||
0.25x0.25 | Maximum difference = 3.029404 | -3.908096 : -3.126477 - 1 ( 0.000096%) | ||
0.5x0.5 | Maximum difference = 4.168945 | -4.168945 : -3.335156 - 1 ( 0.000385%) | ||
1.0x1.0 | Maximum difference = 2.676575 | -2.676575 : -2.141260 - 0 ( 0.000000%) |