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This only involves a bounded rotation field for the first case and a bounded strain field for the second case.
We conclude that these effects were caused by upward transport of molecular gas to the lower thermosphere for the first case and a pulldown forcing of molecular species above the low-pressure zone inside the cyclone for the second case.
There are several potential reasons for this as we discussed earlier concerning the limitations, e.g. searches originating elsewhere in the same country for the first case and a lack of Internet access in the second case.
It was concluded that these effects were caused by the upward transport of molecular gas to the lower thermosphere for the first case and a pulldown forcing of molecular species above the low-pressure zone inside the cyclone for the second case.
Similar(55)
For obvious reasons, we expected more hungry participants in the first case and less hungry participants in the second case.
For the first case, since, we get and.
Preoperative preparations were the same as for the first case.
We will present the detailed proof only for the second case (similar arguments apply for the first case).
The first case is for a dry gas reservoir.
The first case study (Case 1) is for a producing well offshore Iran.
In the first case, for all.
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