首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >All-sky radiation over a glacier surface in the Southern Alps of New Zealand: characterizing cloud effects on incoming shortwave, longwave and net radiation
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All-sky radiation over a glacier surface in the Southern Alps of New Zealand: characterizing cloud effects on incoming shortwave, longwave and net radiation

机译:新西兰南阿尔卑斯山冰川表面上的全天辐射:表征云对短波,长波和净辐射的影响

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Clouds are important features of many high-altitude and glaciated areas, yet detecting their presence and specifying their effects on incoming shortwave (SW), longwave (LW) and net all-wave radiation (Rnet) remains challenging in these environments. These limitations hamper efforts to understand atmospheric controls on glacier surface mass balance (SMB) in the Southern Alps of New Zealand, as both cloud and airmass forcing accompanies key synoptic controls on SMB. Multi-year datasets of four-component broadband radiation from two sites at Brewster Glacier, Southern Alps of New Zealand, are used here to develop cloud metrics to account for the effects of clouds on SW, LW and Rnet. On average 23% of top-of-atmosphere shortwave radiation (SWTOA) is attenuated by the clear-sky atmosphere, while clouds attenuate a further 31%, resulting in <50% of SWTOA being received at the surface. The transmission of shortwave radiation by clouds (trc) during overcast conditions is found to vary with season and airmass characteristics. A simple parameterization is developed to account for lower trc observed during periods of higher water vapour pressure. Cloud metrics derived at the site show overcast conditions are frequent (45% of period) and strongly dependent on wind direction, highlighting the dominant role of orography in cloud formation and enhancement in the Southern Alps. The effect of clouds on Rnet exhibits a distinct seasonal variation; during summer when albedo and trc are lower, clouds decrease Rnet by 20-40Wm(-2), while during autumn, winter and spring, clouds enhance Rnet by approximately 20Wm(-2). Idealized modelling shows that these patterns are strongly dependent on albedo and extend across the elevation range of glaciers in the Southern Alps. Thus, overcast conditions appear to aid the extension of ablation into spring and autumn by increasing the energy available for snow and ice melt.
机译:云是许多高海拔和冰川地区的重要特征,但是在这些环境中,检测云的存在并确定其对入射短波(SW),长波(LW)和净全波辐射(Rnet)的影响仍然具有挑战性。这些局限性阻碍了人们对新西兰南部阿尔卑斯山对冰川表面质量平衡(SMB)大气控制的理解,因为云和气团强迫都伴随着对SMB的关键天气控制。来自新西兰南阿尔卑斯山布鲁斯特冰川两个站点的四分量宽带辐射的多年数据集在这里用于开发云度量标准,以说明云对西南偏北,西南偏北和南北偏东的影响。晴空大气平均衰减了大气顶部短波辐射(SWTOA)的23%,而云层又衰减了31%,导致地面接收不到<50%的SWTOA。在阴天条件下,云层(trc)的短波辐射传输随季节和气团特征而变化。开发了一种简单的参数化方法,以解决在较高水蒸气压力期间观察到的较低trc的问题。从站点获得的云度量表明阴云天气很频繁(占周期的45%),并且强烈依赖于风向,​​突出了地形学在南阿尔卑斯山云形成和增强中的主导作用。云对Rnet的影响表现出明显的季节性变化;在反照率和trc较低的夏季,云使Rnet减小20-40Wm(-2),而在秋季,冬季和春季,云使Rnet增大约20Wm(-2)。理想化的模型表明,这些模式强烈依赖于反照率,并且在南阿尔卑斯山的冰川高程范围内延伸。因此,阴天条件似乎通过增加可用于雪和冰融化的能量来帮助将消融扩展到春季和秋季。

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