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b Storm relative helicity (SReH; horizontal axis) and low-level water vapor at the height of 0.8 km (vertical axis).
This difference in low-level water vapor between #004 and #007 might be one reason why intense vorticity was not generated in #007.
The temporal variations of intense vortices and the horizontal distributions of environmental factors (e.g., low-level water vapor and vertical shear of horizontal winds) are examined in this section to show how environmental factors affect intense vortex generation.
a The vertical shear of horizontal wind (ΔUV) between the heights of 0.8 and 2.5 km (horizontal axis) and low-level water vapor (Qv) at the height of 0.8 km (vertical axis).
Comparison of the multiple possible scenarios showed that the duration of the southernmost tornado was related to the low-level water vapor and the vertical wind shear between heights of 0.8 and 2.5 km.
More importantly, The dye is found to serve as supersensitive fluorescent indicator for the quantitative detection of low-level water content in five common organic solvents with low detection limits.
The distributions of low-level water vapor show that a humid region also existed on the eastern side of the rainfall regions in both members #004 and #007 and that more water vapor was supplied to the rainfall regions in #004 than in #007 (Fig. 12c, d).
We therefore examined the horizontal distributions of the vertical shear of horizontal winds and of the low-level water vapor at 11 40 JST (5 min before the outbreak of the reproduced southernmost intense vortex in #004) reproduced by #004 and #007 to see where the differences existed between them (Fig. 12).
Storm tides reached 7.81 feet (2.4 m) above the mean low-level water mark along Fripp Island, leading to some beach erosion along portions of the coastline.
At least 350 km of major waterways and tributaries in the Swan-Avon Basin were found to exhibit base-flow acidity (pH < 4.5) along with low-level waters in a number of lakes.
Therefore, they prevent large clusters at a low level of water.
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Justyna Jupowicz-Kozak
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