首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing >Comparison of Model Predictions With Measurements of Ku- and Ka-Band Near-Nadir Normalized Radar Cross Sections of the Sea Surface From the Genesis and Rapid Intensification Processes Experiment
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Comparison of Model Predictions With Measurements of Ku- and Ka-Band Near-Nadir Normalized Radar Cross Sections of the Sea Surface From the Genesis and Rapid Intensification Processes Experiment

机译:从创世和快速强化过程实验比较模型预测与测量海面Ku波段和Ka波段近天底归一化雷达截面

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A comparison of model predictions with measurements of near-nadir normalized radar cross sections (NRCSs) of the sea surface at Ku- and Ka-bands is reported. Measurements of Airborne Precipitation Radar Second Generation (APR-2) from near nadir to 25$^{circ}$ incidence angle, along with simultaneous wind truth from dropsonde observations, are compared with predictions of the “cutoff-invariant” two-scale model of sea scattering with the overall goal of assessing the model for possible future use in the APR-2 calibration process. The performance of the model as a function of wind speed and incidence angle is therefore emphasized. The measured data set, acquired primarily during the 2010 “Genesis and Rapid Intensification Processes” (GRIP) experiment, includes wind speeds from approximately 5 to 45 m/s. Model comparisons are limited by uncertainties in the wind fields due to limited dropsonde coverage; the data set is separated into “more reliable” (containing wind speeds of 5–20 m/s) and “less reliable” (wind speeds of 5–45 m/s) wind truth categories accordingly. Because a model of the sea spectrum is required for cutoff-invariant model predictions, comparisons with measured data are performed for three differing sea spectrum descriptions. It is found that a bias of less than $sim$ 1 dB over the wind speed range 5–40 m/s and a standard deviation less than 1 dB over the wind speed range 10–40 m/s can be achieved when using the “unified” sea spectrum description of Elfouhaily The model also provides error levels that are near uniform with respect to both incidence angle and wind speed.
机译:报告了模型预测与Ku和Ka波段海面近天底归一化雷达截面(NRCS)的测量值的比较。将近天底到入射角25°的机载降水雷达第二代(APR-2)的测量值与探空仪观测的同时风真相进行了比较,并与“截止不变”两尺度模型的预测进行了比较海洋散射的总体目标是评估模型,以备将来在APR-2校准过程中使用。因此,该模型的性能取决于风速和入射角。主要在2010年的“创世纪和快速集约化过程”(GRIP)实验中获得的测量数据集包括大约5至45 m / s的风速。由于空投探空仪的覆盖范围有限,模型比较受到风场不确定性的限制;相应地,数据集分为“更可靠”(风速为5–20 m / s)和“较不可靠”(风速为5–45 m / s)风真类别。由于海域光谱模型对于临界不变模型预测是必需的,因此针对三种不同的海域光谱描述与测量数据进行比较。结果发现,使用风速为5–40 m / s时,偏差小于$ sim $ 1 dB,风速为10–40 m / s时,标准偏差小于1 dB。 Elfouhaily的“统一”海谱描述该模型还提供了相对于入射角和风速几乎一致的误差水平。

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