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In between these two estimates are Jianhua Zhang, Chunxia Jiang and Peng Wang, two of whom are with the People's Bank of China.
However, these two estimates are only marginally significant.
These two estimates combined together imply (3.18) for (epsilon>0) sufficiently large.
These two estimates were important to constrain the extent of the desalination of the system.
In order to compare these two estimates, consider the simplest situation.
Combining these two estimates, we obtain T ( r, f ) = S ( r, f ).
These two estimates combined together give (3.18) for (epsilon>0) large.
The correlation coefficient is 0.973, indicating a high similarity between these two estimates.
By putting these two estimates together, we obtain (3.18) for (epsilon>0) large enough.
For daily observations the relative difference between these two estimates stood less than 9%.
Figure 5 shows that these two estimates differ significantly, with the unweighted estimate being higher except for m ≤ 2.5.
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CEO of Professional Science Editing for Scientists @ prosciediting.com