Troposphere delay modeling in SLR based on PMF, VMF3o, and meteorological data

IF 3.5 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Progress in Earth and Planetary Science Pub Date : 2024-03-07 DOI:10.1186/s40645-024-00613-2
Mateusz Drożdżewski, Krzysztof Sośnica
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Abstract

Satellite laser ranging (SLR) requires accurate troposphere delay models to properly correct the observed distances to satellites and derive fundamental geodetic and geodynamic parameters. The currently used models for the tropospheric delay employ in situ meteorological data collected simultaneously with laser measurements. However, the standard models assume full symmetry of the atmosphere above the SLR stations because all meteorological data come from one sensor. In this study, we evaluate various methods of troposphere delay modeling based on numerical weather models, such as the Potsdam Mapping Function (PMF) and Vienna Mapping Function for optical frequencies (VMF3o), in situ measurements, the Wrocław gradient model (WGM) and the combination of different models. We found large discrepancies between pressure, temperature, and humidity records between in situ measurements and numerical models. The best results for the zenith delays are obtained when using in situ meteorological data with the estimation of tropospheric biases. For stations with some deficiencies in proper humidity measurements, e.g., Zimmerwald in Switzerland, the best results are obtained when using hydrostatic zenith delays based on in situ data and wet delays based on numerical weather models. Finally, we found that using horizontal gradients of the tropospheric delay is indispensable to avoid biases in the SLR-based Earth rotation parameters of approximately 20 \(\upmu\)as for polar motion. The horizontal gradients successfully account for the asymmetry of the troposphere above SLR stations and can be derived from PMF, VMF3o, or a parameterized WGM model with similar accuracies.

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基于 PMF、VMF3o 和气象数据的可持续土地退化中的对流层延迟建模
卫星激光测距(SLR)需要精确的对流层延迟模型,以正确校正观测到的卫星距离,并推导出基本的大地测量和地球动力参数。目前使用的对流层延迟模型采用了与激光测量同时收集的现场气象数据。然而,由于所有气象数据都来自一个传感器,因此标准模型假定可持续轨道站上方的大气层完全对称。在这项研究中,我们评估了基于数值天气模式的对流层延迟建模的各种方法,如波茨坦绘图函数(PMF)和维也纳光学频率绘图函数(VMF3o)、原位测量、弗罗茨瓦夫梯度模式(WGM)以及不同模式的组合。我们发现,实地测量和数值模式之间的气压、温度和湿度记录存在很大差异。利用对流层偏差估算的原地气象数据可获得天顶延迟的最佳结果。对于湿度测量不准确的站点,如瑞士的齐默瓦尔德,使用基于原地数据的静力学天顶延迟和基于数值天气模式的湿延迟可获得最佳结果。最后,我们发现,使用对流层延迟的水平梯度对于避免基于 SLR 的地球自转参数中约 20 \(\upmu\)的极地运动偏差是不可或缺的。水平梯度成功地解释了SLR站点上方对流层的不对称性,可以从PMF、VMF3o或参数化的WGM模型中得出,精度相似。
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来源期刊
Progress in Earth and Planetary Science
Progress in Earth and Planetary Science Earth and Planetary Sciences-General Earth and Planetary Sciences
CiteScore
6.50
自引率
5.10%
发文量
59
审稿时长
31 weeks
期刊介绍: Progress in Earth and Planetary Science (PEPS), a peer-reviewed open access e-journal, was launched by the Japan Geoscience Union (JpGU) in 2014. This international journal is devoted to high-quality original articles, reviews and papers with full data attached in the research fields of space and planetary sciences, atmospheric and hydrospheric sciences, human geosciences, solid earth sciences, and biogeosciences. PEPS promotes excellent review articles and welcomes articles with electronic attachments including videos, animations, and large original data files. PEPS also encourages papers with full data attached: papers with full data attached are scientific articles that preserve the full detailed raw research data and metadata which were gathered in their preparation and make these data freely available to the research community for further analysis.
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