EMOSLIB does not apply any land sea-mask processing when interpolating the mean sea-level pressure so differences arise only from the different interpolation method and selection of nearest points used by MIR
HRES O1280
Mean sea-level pressure has been interpolated from the O1280 octahedral reduced Gaussian grid to regular lat-lon grids at different target resolutions using EMOSLIB and MIR.
- The differences for more than 99% of grid points are less than 20Pa and in the cases presented here all differences are less than 1 hPa.
- The largest differences occur in regions of high orography with the field gradient changes most rapidly.
- Larger differences are also seen in the lower resolution target grids (0.5ºx0.5º and 1.0ºx1.0º) at the polar latitudes (90ºN and 90ºS) which arise from the different handling of the interpolation at the poles.
The plots show the differences with the contours chosen on a logarithmic scale to enhance the smaller differences. Differences smaller than 0.1% of the field range are not shown. 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 circles.
Target resolution | Statistics of differences | Histogram of differences | Global | Europe |
---|---|---|---|---|
0.1x0.1 | Maximum difference = 68.125000 |
Mean
Mean absolute difference = |
0. |
312304 |
0.125000 |
RMS of differences = 1. |
072257 |
Percentage of points with absolute difference < 1.0 = 95.306% | -100.0 : -90.0 - 1 ( 0.000015%) |
70. |
0 : - |
60. |
0 - |
5 ( 0. |
000077%) |
60. |
0 : - |
50. |
0 - |
12 ( 0. |
000185%) |
( 0.000555%) |
009840%) |
20. |
0.000000 : 18.275000 - 3179303 ( 49.036076%)
18.275000 : 36.550000 - 932 ( 0.014375%)
6.550000 : 54.825000 - 72 ( 0.001110%)
54.825000 : 73.100000 - 9 ( 0.000139%)
73.100000 : 91.375000
0 : -10.0 - 7583 ( 0.116957%) |
0.125x0.125 | Maximum difference = 92.937500 |
Average difference = -0.000149
|
0. |
297040 |
0.062500 |
RMS of differences = 1. |
112258 |
Percentage of points with absolute difference < 1.0 = 95.244% | -100.0 : -90.0 - 0 ( 0.000000%) |
50. |
0 : - |
40. |
0 - |
26 ( 0. |
000626%) |
40. |
0 : - |
30. |
0 - |
84 ( 0. |
002024%) |
30. |
0 : - |
20. |
0 - |
387 ( 0.009325%) |
131226%) |
10. |
0 : |
0. |
0 - |
2862191 ( |
68. |
967128%) |
0. |
0 : |
10. |
0 - |
1276136 ( 30. |
749672%) |
10. |
0 : 20.0 - 5303 ( 0.127781%) |
008723%) |
30. |
0 : 40.0 - 81 ( 0.001952%) |
000048%) |
70. |
0 : 80.0 - 3 ( 0.000072%) |
000000%) |
90. |
0 : |
100. |
0 - |
1 ( 0. |
000024%) |
0.25x0.25 | Maximum difference = 92.875000 |
Mean absolute difference = 0. |
338583 |
0.125000 |
RMS of differences = 1. |
266861 |
Percentage of points with absolute difference < 1.0 = 95.149% | -100.0 : -90.0 - 0 ( 0.000000%) |
-70.0 : -60.0 - 4 ( 0.000385%) |
40. |
0 : - |
30. |
0 - |
15 ( 0. |
001445%) |
30. |
0 : - |
20. |
0 - |
101 ( 0.009728%) |
196775%) |
10. |
0 : 0. |
0 - |
527362 ( 50. |
793843%) |
0. |
0 : |
10. |
0 - |
506516 ( 48. |
18.575000 : 37.150000 - 141
786022%) |
008957%) |
30. |
0 : |
40. |
0 - 19 ( 0.001830%) |
000096%) |
70. |
0 : |
80. |
0 - 1 ( 0.000096%) |
80.0 : 90.0 - 0 ( 0.000000%) |
000096%) |
0.5x0.5 | Maximum difference = 51.000000 |
Average difference = 0.004363
|
309541 |
RMS of differences = 1.523153 Percentage of points with absolute difference < 1.0 = 94.304% | -70.0 : -60.0 - 2 ( |
0.000769%) |
000385%) |
40. |
0 : - |
30. |
0 - |
3 ( 0. |
001154%) |
30. |
0 : - |
20. |
0 - |
21 ( 0. |
008079%) |
20. |
0 : - |
10. |
0 - |
855 ( 0. |
328947%) |
10. |
0 : 0. |
0 - |
41886 ( 16. |
114958%) |
0. |
0 : |
10. |
0 - |
216238 ( 83. |
194060%) |
10. |
0 : |
20. |
0 - |
871 ( 0. |
335103%) |
20. |
0 : |
30. |
0 - |
33 ( 0.012696%) |
002308%) |
40. |
0 : |
50. |
0 - |
2 ( 0. |
000769%) |
50. |
0 : |
60. |
0 - 1 ( 0.000385%) |
1.0x1.0 | Maximum difference = 50.937500 |
Average difference = 0.012001
|
437874 |
0.062500 |
RMS of differences = 1.932777 |
Percentage of points with absolute difference < 1.0 = 94.672% | -70.0 : -60.0 - 1 ( 0.001535%) |
60.0 : -50.0 - 0 ( 0.000000%) |
40. |
0 : - |
30. |
0 - 0 ( 0.000000%) |
20. |
0 : - |
10. |
0 - |
389 ( 0. |
596992%) |
10. |
0 : 0. |
0 - |
44619 ( 68. |
476059%) |
0 : |
10. |
0 - |
19737 ( 30. |
290055%) |
10. |
0 : |
20. |
0 - |
401 ( 0. |
615408%) |
20.0 : 30.0 - 9 ( 0.013812%) |
001535%) |
40. |
0 : |
50. |
0 - 0 ( 0.000000%) |
50. |
0 : 60. |
0 - 1 ( 0.001535%) |