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Arctic ice clouds over northern Sweden: microphysical properties studied with the Balloon-borne Ice Cloud particle Imager B-ICI

机译:瑞典北部上空的北极冰云:用气球传播的冰云粒子成像仪B-ICI研究的微观物理性质

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Ice particle and cloud properties such as particle size, particle shape and number concentration influence the net radiation effect of cirrus clouds. Measurements of these features are of great interest for the improvement of weather and climate models, especially for the Arctic region. In this study, balloon-borne in?situ measurements of Arctic cirrus clouds have been analysed for the first time with respect to their origin. Eight cirrus cloud measurements have been carried out in Kiruna (68 sup°/sup N), Sweden, using the Balloon-borne Ice Cloud particle Imager (B-ICI). Ice particle diameters between 10 and 1200 μm have been found and the shape could be recognized from 20 μm upwards. Great variability in particle size and shape is observed. This cannot simply be explained by local environmental conditions. However, if sorted by cirrus origin, wind and weather conditions, the observed differences can be assessed. Number concentrations between 3 and 400?L sup?1/sup have been measured, but the number concentration has reached values above 100?L sup?1/sup only for two cases. These two cirrus clouds are of in?situ origin and have been associated with waves. For all other measurements, the maximum ice particle concentration is below 50?L sup?1/sup and for one in?situ origin cirrus case only 3?L sup?1/sup . In the case of in?situ origin clouds, the particles are all smaller than 350 μm diameter. The PSDs for liquid origin clouds are much broader with particle sizes between 10 and 1200 μm . Furthermore, it is striking that in the case of in?situ origin clouds almost all particles are compact (61?%) or irregular (25?%) when examining the particle shape. In liquid origin clouds, on the other hand, most particles are irregular (48?%), rosettes (25?%) or columnar (14?%). There are hardly any plates in cirrus regardless of their origin. It is also noticeable that in the case of liquid origin clouds the rosettes and columnar particles are almost all hollow.
机译:冰粒和云的性质(例如粒径,颗粒形状和数量浓度)会影响卷云的净辐射效应。这些特征的测量对于改善天气和气候模型,特别是对北极地区而言,具有极大的意义。在这项研究中,首次对北极卷云的气球传播原位测量进行了分析。使用气球载冰云粒子成像仪(B-ICI)在瑞典基律纳(N <68)进行了八次卷云测量。已经发现冰的粒径在10至1200μm之间,并且从20μm以上可以识别出冰的形状。观察到粒径和形状的巨大变化。这不能简单地用当地的环境条件来解释。但是,如果按卷云的起源,风和天气条件进行分类,则可以评估观察到的差异。测量了3至400?L ?1 之间的数字浓度,但仅在两种情况下,数字浓度达到100?L ?1 以上的值。这两个卷云起源于原地,并与海浪有关。对于所有其他测量,最大冰粒浓度都在50?L ?1 以下,而对于一个原位起源的卷云,则只有3?L ?1 。在原位云的情况下,粒子直径均小于350μm。液态云的PSD范围更广,粒径在10至1200μm之间。此外,令人惊讶的是,在异地起源云的情况下,当检查粒子形状时,几乎所有粒子都是致密的(61%)或不规则的(25%)。另一方面,在液态云中,大多数颗粒是不规则的(48%),莲座状(25%)或柱状(14%)。卷云几乎没有板块,无论其来源如何。还值得注意的是,在液体起源的云的情况下,玫瑰花结和柱状颗粒几乎都是空心的。

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