In doing so, we concentrate on the large-scale, wind-driven flow of the mid-latitude oceans, which is dominated by the presence of a larger, anticyclonic and a smaller, cyclonic gyre.
It accelerated to the northeast under the flow of the mid-latitudes, and the typhoon weakened more rapidly; JMA downgraded Isa to a tropical storm on April 22, which was followed suit by the JTWC the next day as upper-level wind shear increased.
Recent studies suggest the existence of a 'channel flow' in the mid- to lower crust of the plateau which might explain the varying and complex deformation of the Tibetan plateau (Bai et al. 2010; Clark and Royden 2000).
For the details of the Copula function, readers can refer to [22]. Figure 4 shows the flow chart of the mid-short-term risk assessment that considers the external environment, the health of the component, load fluctuations, and generating unit outages.
Changes in the anomalous secondary circulation, namely anomalous upward (downward) flow in the SWNP and anomalous downward (upward) flow in the mid-latitudes of East Asia, are one of the causes of drought (non-drought).
The previous studies focus on the channeling-induced low-level jet; Wu et al. (2015) proposed that the leading role of the northerly asymmetric flow in the mid-troposphere causing the southward deflection of the simulated TC tracks; overall, their deep-layer areal-mean asymmetric flow is consistent with the movement of storm, although some discrepancy still exists.
IZO is influenced by flow from both the mid-latitudes and the subtropics and NAO changes have resulted in an increased flow of the Westerlies in the mid-latitude subtropical North Atlantic, thus favoring the transport of O3 and its precursors from North America.
The Atchafalaya, via the Old River, threatens to capture the major flow of the Mississippi; since the mid-20th century, however, a navigable system of dams, locks, and levees has kept the waters in check.
In contrast to the baseline flow, where the flow field was fully separated, the two-dimensional control jet was able to eliminate flow separation at the mid-span portion of the duct and changed considerably the three-dimensional flow field, and ultimately, the inlet performance.
It is demonstrated that the widely used assumption of two-dimensional flow field in the mid-span leads to serious overestimation of the suction pressures over the roof and on the leeward wall.
All groups had elevated differences between thoracic and mouth flows in the mid-fraction of forced expiratory manoeuvre.
