利用gnss -反射法监测北极海平面变化

Su‐Kyung Kim, Jihye Park
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引用次数: 5

摘要

由于北极地区对全球气候和生态系统有重大影响,因此长期和短期的水位变化对北极至关重要。水位变化通常由潮汐计监测。然而,由于极端的环境,在北极安装和维护潮汐计以获得连续和无缝的水位数据是具有挑战性的。在本研究中,我们研究了GNSS-Reflectometry (GNSS-R)作为一种替代的北极水位监测方法,该方法基于遥感技术测量水位。由于卫星几何形状和电离层对GNSS信号的影响导致GNSS在高纬度地区的性能下降,因此采用了增强型GNSS- r算法,该算法通过基于GNSS(包括GPS和伽利略)的多频率增强频谱分析和统计可靠性验证来准确确定海平面。此外,通过包括伽利略,可见卫星的数量也增加了,这解决了高纬度地区缺乏可用观测的另一个挑战。通过分析2018年6月阿拉斯加圣迈克尔的水位变化,验证了所建议的算法。将基于GNSS-R的潮汐仪得到的水位与相邻的两个NOAA的St. Michael和Unalakleet潮汐仪(ID: 9468132和9468333)分别约1.5 km和74 km的独立数据进行比较。结果表明,两者具有较好的一致性,相关系数高达0.87。此外,通过频谱分析,从GNSS-R测潮仪测量的海平面变化中得到了有意义的谐波分量、M2、K1和O1。此外,通过加入伽利略卫星,输出的时间分辨率显着提高。通过实施先进的GNSS-R算法,该研究成功地测量了环境挑战性地区的高精度和精确的水位变化。实验结果表明,基于GNSS-R的北极测潮仪具有广泛的应用前景。
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Monitoring Sea Level Change in Arctic using GNSS-Reflectometry
Long- and short-term variation of water level is critical in the Arctic as this region significantly affects the global climate and ecosystems. The water level changes are conventionally monitored by a tidal gauge. However, installing and maintaining tide gauges for continuous and seamless water level data in the Arctic is challenging due to the extreme environment. In this study, we investigate GNSS-Reflectometry (GNSS-R) as an alternative water level monitoring method in the Arctic, which measures the water levels based on remote sensing technique. Since GNSS performance at high latitudes is degraded due to satellite geometry and ionospheric effects on GNSS signals, an enhanced GNSS-R algorithm is applied, which accurately determines sea levels through enhanced spectrum analysis based on GNSS - including GPS and Galileo - multiple frequencies and statistical reliability verification. In addition, by including Galileo, the number of visible satellites is also increased that tackles another challenge of lack of available observations at high latitudes. The suggested algorithms are validated by analyzing water level changes in St. Michael, Alaska in June 2018. The water levels derived by GNSS-R based tide gauge are compared to independent data from the two neighboring NOAA’s St. Michael and Unalakleet tide gauges (ID: 9468132 and 9468333) about 1.5 km and 74 km of GNSS-R based tide gauge, respectively. As a result, a good agreement is confirmed with a high correlation coefficient of up to 0.87. In addition, from a spectral analysis, meaningful harmonic constituents, M2, K1, and O1 are founded from the sea level changes measured by GNSS-R based tide gauge. In addition, the temporal resolution of the output was significantly increased by adding the Galileo satellites. By implementing the advanced algorithms of GNSS-R, the proposed study successfully measured the highly accurate and precise water level variation in an environmentally challenging region. The experimental results show many promising applications for the Arctic GNSS-R based tide gauge.
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