WebMar 21, 2007 · [1] Interannual variations of high potential vorticity intrusions at 10°S in the upper troposphere during NDJFM are shown to be negatively correlated with rainfall over northern northeast Brazil (NEB). That is, higher intrusions associated with stronger equatorial westerlies may provoke droughts. Higher intrusions lead to the formation of an … WebApr 12, 2024 · Interestingly, a delaying and limited increasing trend in the high-level potential temperature similar to the low-level vorticity can also be found in Figure 11. For the …
Interannual variability of high potential vorticity in South Atlantic ...
WebJul 5, 2011 · There are high values of PV (−1.5 PVU) extending toward the tropical region near 25°W, forming a ‘tongue’ of HIGH-PV northwest–southeast. This incursion of HIGH-PV in the tropics occurs in the vicinity of the western equatorial ‘ducts’. The Um at 10°S has values exceeding 10 m s −1 between 40°W and 20°W. Webatures, high baryochemical potential region, the phase transition becomes a rst-order one. These phase transi-tion lines meet at a hypothesized critical endpoint (CEP), ... vorticity circling the longitudinal axis in the system [26{31]. … fly navy football helmet
Abnormal warm sea‐surface temperature in the Indian Ocean, …
WebJun 1, 2000 · This front separates a region of very low homogeneous potential vorticity on the equatorward side from a homogeneous high potential vorticity region on the poleward side. Each potential vorticity pool extends well beyond the … Within the troposphere, the values of PV are usually low. However, the potential vorticity increases rapidly from the troposphere to the stratosphere due to the significant change of the static stability. Typical changes of the potential vorticity within the area of the tropopause are from 1 (tropospheric air) to … See more Situation (b) is the appearance in the WV imagery in the case of a frontal zone. Most striking here is the shape of the PV-anomaly: The tropopause has been folded in this situation. This … See more The values of the PV are characterised, as described above, by increasing values from south to north. The anomaly of the PV, the area where the … See more WebDiabatic generation of negative potential vorticity and its impact on the North Atlantic jet stream . × ... The fine-scale structure noted in the in situ wind data of Fig. 4a is also clearly evident in Fig. 4b as bands of high vorticity, of too small a scale to be captured by the dropsondes. Fig. 4c shows that the ozone concentration along the ... greenon the golf watch zeal