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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Comparisons of global cloud ice from MLS, CloudSat,and correlative data sets
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Comparisons of global cloud ice from MLS, CloudSat,and correlative data sets

机译:来自MLS,CloudSat和相关数据集的全球云冰的比较

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摘要

Aura Microwave Limb Sounder (MLS) version 2.2 (V2.2) and CloudSat R04(release 4) ice water content (IWC) and partial-column ice water path (pIWP)measurements are analyzed and compared to other correlative data sets. The MLS IWC,representing an average over —300 x 7 x 4 km3 volume, is retrieved at 215-268 hPawith precision varying between 0.06 and 1 mg/m3. The MLS pIWP products,representing the partial columns over 100 x 7 km2 area with the bottom at —8, —6, and11 km for 115, 240, and 640 GHz, have estimated precisions of 5, 1.5, and0.8 g/m2, respectively. CloudSat, on the other hand, shows a minimum detectablesensitivity of —31 dBZ in the reflectivity measurement at 94 GHz. CloudSat IWC is anaverage over —1.8 x 1.4 x 0.5 km3 volume, and its precision varies from 0.4 mg/m3at 8 km to 1.6 mg/m3 at 12 km. The estimated single-profile precision for CloudSatIWP is —9 g/m2. However, these measurements are associated with relatively largesystematic error, mostly due to uncertainties in the retrieval assumptions aboutmicrophysics, which lead to relatively poor accuracy compared to measurement precision.To characterize systematic differences among various observations and those derived frommodels, we employ the normalized probability density function (pdf) in thecomparisons. CloudSat IWC shows generally consistent slopes of pdf distribution with insitu observations, particularly at —12 km where the in situ data come mostly from long-legflights. Despite similar IWC morphology found between MLS and CloudSatobservations, CloudSat R04 IWC retrieval is higher compared to MLS, especially at14-17 km where the MLS technique is not limited by sensitivity saturation. The MLS andCloudSat IWC pdf's agree well in the overlapped sensitivity range with relative difference<50%, but the difference appears to increase with IWC. MLS and CloudSat cloud icemeasurements are compared with other data sets in terms of monthly map and pdf.Comparisons with European Center for Medium range Weather Forecasting (ECMWF)analyses show that grid box averages of monthly ECMWF IWC are much smaller (by5 x and —20 x) than the same MLS and CloudSat averages. Comparisons of pIWP datafrom CloudSat and passive sensors reveal large uncertainties associated with passivetechniques, such as penetration depth and sensitivity limitation. In particular, retrievalsfrom Moderate Resolution Imaging Spectroradiometer (MODIS) and AdvancedMicrowave Sounding Unit-B (AMSU-B) differ largely in IWP pdf from the CloudSat R04retrieval, showing CloudSat values generally lower (by —5x and —8x, respectively) atIWP = 10-500 g/m2 but higher at IWP > 500 g/m2.
机译:分析了Aura Microwave Limb Sounder(MLS)2.2版(V2.2)和CloudSat R04(版本4)冰水含量(IWC)和部分塔冰水路径(pIWP)测量结果,并将其与其他相关数据集进行了比较。 MLS IWC表示平均体积超过300×7×4 km3,可在215-268 hPa的压力下获取,精度在0.06和1 mg / m3之间变化。 MLS pIWP产品代表115、240和640 GHz处100×7 km2区域的局部色谱柱,其底部分别位于–8,–6和11 km,估计精度为5、1.5和0.8 g / m2 , 分别。另一方面,CloudSat在94 GHz的反射率测量中显示的最小可检测灵敏度为–31 dBZ。 CloudSat IWC的平均体积为— 1.8 x 1.4 x 0.5 km3,其精度从8 km时的0.4 mg / m3到12 km时的1.6 mg / m3不等。 CloudSatIWP的估计单轮廓精度为—9 g / m2。但是,这些测量与相对较大的系统误差有关,这主要是由于有关微观物理学的检索假设存在不确定性,与测量精度相比,其准确性相对较差。为了表征各种观测值与模型得出的观测值之间的系统差异,我们采用归一化概率密度比较功能(pdf)。 CloudSat IWC显示的pdf分布斜率与实地观测值基本一致,尤其是在12 km处,那里的实地数据主要来自长途飞行。尽管在MLS和CloudSatobservations之间发现了类似的IWC形态,但是CloudSat R04 IWC的检索比MLS更高,尤其是在14-17 km,MLS技术不受灵敏度饱和度的限制。 MLS和CloudSat IWC pdf在重叠灵敏度范围内相吻合,相对差异<50%,但差异似乎随着IWC的增加而增加。将MLS和CloudSat云的冰面积与每月地图和pdf的其他数据集进行了比较。与欧洲中距离天气预报中心(ECMWF)的分析比较表明,每月ECMWF IWC的网格框平均值小​​得多(分别为5倍和-20) x)比相同的MLS和CloudSat平均值高。来自CloudSat和被动传感器的pIWP数据的比较显示,与被动技术相关的不确定性很大,例如穿透深度和灵敏度限制。特别是,从中等分辨率成像光谱仪(MODIS)和AdvancedMicrowave Sounding-B(AMSU-B)检索到的IWP pdf与CloudSat R04检索的IWP pdf有很大不同,显示在IWP = 10时,CloudSat值通常较低(分别降低了–5倍和-8倍)。 -500 g / m2,但在IWP> 500 g / m2时更高。

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