Deep Rybka 5 [BETTER] – Know Thy Country

Deep Rybka 5

The following limitations in Deep Rybka 5 are listed:

Weak
No
No
No
No

Bulk-material mineral deposits are very important for understanding both the global and local impacts of climate change on the Earth. There are currently only four sites on Earth where this information is available: the Porcupine Maple Glaciopile, the Gonzalez Dome, the Anguillan Highlands, and the Antarctic Dome. In contrast, there are almost 500 sites on the Greenland Ice Sheet where the effects of melting ice loss from snowfall and snowmelt are only beginning to be understood. We have constructed a numerical ice sheet model of the Greenland Ice Sheet that includes the effects of freezing and melting from both snowfall and snowmelt. The model has been applied to predict the effect of ice loss on the Greenland Ice Sheet and to reconstruct the timing and locations of Arctic glacial lakes. The results indicate that approximately 0.5+-0.1mm/year of the now-abating Arctic ice sheet is still sequestered and, thus, we predict that Arctic glacial lakes will keep growing if the melt water-flux continues.

Rybka 4.2 is a successor program of Rybka 5. This successor program was the successor program of Rybka 4. Rybka 4.2 is, therefore, the successor of a successor program. It is the successor of Rybka 4, which is the successor of Rybka 3. Rybka 3 is the successor of Rybka 2. Rybka 2 is the successor of Rybka 1. Rybka 1 is the successor of Rybka 0.

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