Young Zachary M, Blewitt Geoffrey, Kreemer Corné
Nevada Bureau of Mines and Geology, University of Nevada, 1664 N Virginia St. MS 178, Reno, NV 89557 USA.
Department of Geosciences, University of Montana, 32 Campus Dr., Missoula, MT 59812 USA.
J Geod. 2024;98(10):89. doi: 10.1007/s00190-024-01898-3. Epub 2024 Oct 7.
Accurate positioning using the Global Positioning System relies on accurate modeling of tropospheric delay. Estimated tropospheric delay must vary sufficiently to capture true variations; otherwise, systematic errors propagate into estimated positions, particularly the vertical. However, if the allowed delay variation is too large, the propagation of data noise into all parameters is amplified, reducing precision. Here we investigate the optimal choice of tropospheric constraints applied in the GipsyX software, which are specified by values of random walk process noise. We use the variability of 5-min estimated positions as a proxy for tropospheric error. Given that weighted mean 5-min positions closely replicate 24-h solutions, our ultimate goal is to improve 24-h positions and other daily products, such as precise orbit parameters. The commonly adopted default constraint for the zenith wet delay (ZWD) is 3 mm/√(hr) for 5-min data intervals. Using this constraint, we observe spurious wave-like patterns of 5-min vertical displacement estimates with amplitudes ~ 100 mm coincident with Winter Storm Ezekiel of November 27, 2019, across the central/eastern USA. Loosening the constraint suppresses the spurious waves and reduces 5-min vertical displacement variability while improving water vapor estimates. Further improvement can be achieved when optimizing constraints regionally, or for each station. Globally, results are typically optimized in the range of 6-12 mm/√(hr). Generally, we at least recommend loosening the constraint from the current default of 3 mm/√(hr) to 6 mm/√(hr) for ZWD every 300 s. Constraint values must be scaled by √(/300) for alternative data intervals of seconds.
The online version contains supplementary material available at 10.1007/s00190-024-01898-3.
使用全球定位系统进行精确定位依赖于对流层延迟的精确建模。估计的对流层延迟必须有足够的变化以捕捉真实变化;否则,系统误差会传播到估计位置,尤其是垂直方向。然而,如果允许的延迟变化太大,数据噪声向所有参数的传播会被放大,从而降低精度。在这里,我们研究了在GipsyX软件中应用的对流层约束的最佳选择,这些约束由随机游走过程噪声值指定。我们使用5分钟估计位置的变异性作为对流层误差的代理。鉴于加权平均5分钟位置能紧密复制24小时解,我们的最终目标是改善24小时位置和其他每日产品,如精确轨道参数。对于天顶湿延迟(ZWD),常用的默认约束是在5分钟数据间隔内为3毫米/√(小时)。使用这个约束,我们观察到2019年11月27日冬季风暴以西结期间,美国中部/东部5分钟垂直位移估计出现了虚假的波状模式,振幅约为100毫米。放宽约束可抑制虚假波,并减少5分钟垂直位移变异性,同时改善水汽估计。在区域或每个站点优化约束时可进一步改善。在全球范围内,结果通常在6 - 12毫米/√(小时)范围内得到优化。一般来说,我们至少建议将ZWD每300秒的约束从当前默认的3毫米/√(小时)放宽到6毫米/√(小时)。对于秒的替代数据间隔,约束值必须乘以√(/300)进行缩放。
在线版本包含可在10.1007/s00190-024-01898-3获取的补充材料。