By Bohning D.
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Additional info for A comparison of non-iterative and iterative estimators of heterogeneity variance for the standardize
For comparison, the range of elevation on Earth is only 20 kilometers. The large blue circle in the southern hemisphere represents the Hellas impact basin, one of the biggest craters in the solar system. Girdling Hellas is a vast ring of highlands about two kilometers in elevation. 0 2 4 6 8 10 Epithermal Neutron Flux (counts per second) CRUSTAL THICKNESS Combining the topographic map with measurements of Mars’s gravity, researchers have deduced the thickness of the Martian crust: roughly 40 kilometers under the northern plains and 70 kilometers under the far southern highlands.
Part of this benefit arises because the test circuits allow designers to inject “failures” artificially to verify that the chip detects and recovers from them correctly. Our group proposes a software equivalent for computer systems. When operators employed the selective-rebooting strategy, for example, test errors would help determine which software components to reinitialize to counter a particular kind of failure. If the problem propagated to only one or two other elements, operators could reboot only those.
On slopes, the icy mantle shows signs of having flowed like a viscous fluid, much in the manner of a terrestrial glacier. This mantle is becoming the focus of intense scientific scrutiny. Second, Mars is extremely windy. It is dominated by aeolian activity in much the way that Earth is dominated by the action of liquid water. Spacecraft have seen globe-encircling dust storms, huge dust devils and dust avalanches— all wrought by the wind. Dust streaks behind obstacles change with the seasons, presumably because of varying wind conditions.
A comparison of non-iterative and iterative estimators of heterogeneity variance for the standardize by Bohning D.