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Weatherwatch june 2004

机译:Weatherwatch 2004年6月

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The boundary between cool and warm air that helped trigger May downpours in the Midwest shifted south in June. As a result, cooler, drier air gradually overspread the Midwest, while the South became the new focus for heavy rainfall, especially during the second half of June. Rain eased or eliminated the effects of winter and spring dryness in the Southeast, but .caused sporadic flooding from southern and eastern Texas to the Delta. Rainfall also increased in coverage and intensity across the southern half of the Plains. Farther north, however, long-term drought remained deeply entrenched from western Nebraska into southeastern Montana, despite occasional showers. Similarly, scattered showers across the central Rockies and Intermountain West brought superficial improvement but provided little relief from a multi-year drought. Drought-reduced water supplies also remained a concern elsewhere in the West, although a lack of extreme heat helped to limit demands on irrigation reserves.
机译:导致五月中西部地区倾盆大雨的凉爽和温暖的空气之间的界限在6月向南转移。结果,凉爽,干燥的空气逐渐蔓延到中西部,而南部成为新的降雨重点,特别是在六月下半月。降雨缓解或消除了东南部冬季和春季干旱的影响,但造成了德克萨斯州南部和东部到三角洲的零星洪水。平原南部的降雨也增加了覆盖范围和强度。然而,在北部更远的地方,尽管偶尔有阵雨,但长期干旱仍从内布拉斯加州西部到蒙大拿州东南部已根深蒂固。同样,洛矶山脉中部和西部山间地区的零星阵雨带来了表面改善,但多年干旱却无济于事。干旱减少的水供应在西方其他地方也仍然是一个令人担忧的问题,尽管缺乏极端热量有助于限制对灌溉储备的需求。

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