From Observations to Forecasts ‐ Part 13: The UK weather radar network – past, present and future
From Observations to Forecasts ‐ Part 13: The UK weather radar network – past, present and future
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从观测到预测 - 第 13 部分：英国天气雷达网络 - 过去、现在和未来
DOI：
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发表时间：
2011
期刊：
影响因子：
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通讯作者：
A. Illingworth
中科院分区：
文献类型：
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作者：
M. Kitchen;A. Illingworth
布里顿，2010年。英国气象局关于康沃尔洪灾的报道：“并不是所有的预测都是绝对正确的”，《每日电讯报》，http://www.telegraph.co.uk/news/uknews/8149774/Met-Office-onCornwall-floods-not-every-forecast-willbe-absolutely-correct.html[2010年11月22日访问]。戈尔丁·B，克拉克·P，2005年5月。博斯卡斯尔洪水：2004年8月16日洪水情况的气象分析。天气60：230-235。詹姆斯·PK，布朗宁·卡戴珊1979年。地面冷锋线对流的中尺度结构。Q.J.R.气象台。SoC。105：371-382。更详细的雨带应该可以考虑对较小的河流和河流集水区的警告，尽管运行之间的微小变化表明完美的准确性仍然难以捉摸，在解释模型输出时需要考虑到这一点。
Britten N. 2010. Met Office on Cornwall floods: ‘not every forecast will be absolutely correct’, The Daily Telegraph, http://www.telegraph.co.uk/news/ uknews/8149774/Met-Office-onCornwall-floods-not-every-forecast-willbe-absolutely-correct.html [accessed 22 November 2010]. Golding B, Clark P, May B. 2005. The Boscastle flood: meteorological analysis of the conditions leading to flooding on 16 August 2004. Weather 60: 230–235. James PK, Browning KA. 1979. Mesoscale structure of line convection at surface cold fronts. Q. J. R. Meteorol. Soc. 105: 371–382. rain bands with greater levels of detail it should be possible to consider warnings for smaller stream and river catchment areas, although small changes from run to run suggest perfect accuracy will remain elusive and this needs to be taken on board in the interpretation of model output.