An Experimental Study of the Fluxes in the Tropical Marine Boundary Layer as Part of HARP

热、动量和水分在大气中的重新分布 大气层最低1 - 3公里处（边界层） 对于理解进化和自然的重要性 从局部尺度天气到气候的现象。 存在差距 我们对对流边界层和 伴随而来的对流云重新分配了这些量 在垂直方向。 对于大气数值模式， 重要的是，边界层过程必须精确 参数化。 在1985年的一次实地考察中，首席研究员 研究积云卷吸/消散的性质 在海洋边界层中， 夏威夷。 首席研究员将扩展其先前的工作 将使用结果来测试现有的参数化 海洋边界层 此外，她还计划调查 最近的研究表明，宏观 海洋边界层的性质部分取决于 云凝结核。

The redistribution of heat, momentum and moisture within the lowest one to three kilometers of the atmosphere (boundary layer) is of importance for understanding the evolution and nature of phenomena from local scale weather to climate. There are gaps in our knowledge of exactly how the convective boundary layer and the accompanying convective clouds redistribute these quantities in the vertical. For atmospheric numerical models, it is important that boundary layer processes be accurately parameterized. In an field expedition in 1985, the Principal Investigator studied the nature of entrainment/detrainment in cumulus clouds in the marine boundary layer in rainbands off the coast of Hawaii. The Principal Investigator will extend her previous work will use the results to test existing parameterizations of the marine boundary layer. Further, she also plans to investigate suggestions emanating from recent studies that macroscopic properties of the marine boundary layer are determined in part by cloud condensation nuclei.//