4.6 Article

Tropospheric wet tomography and PPP: Joint estimation from GNSS crowdsourcing data

期刊

ADVANCES IN SPACE RESEARCH
卷 70, 期 8, 页码 2399-2411

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.asr.2022.08.004

关键词

Tomography; PPP; Troposphere; GNSS; Slant wet delay; Water vapor; Crowdsourcing

资金

  1. European Space Agency (ESA)
  2. [NAVISP-EL1-008]

向作者/读者索取更多资源

Water vapor is the dominant greenhouse gas in the atmosphere, impacting weather forecasts and GNSS measurements. A new technique is proposed to estimate water vapor distribution using roving receivers, and even low-quality receiver data like from smartphones can be utilized to improve the estimates.
Water vapor is the dominant greenhouse gas in the atmosphere accounting for 50 to 70% of the total effect, it plays a large role in determining the weather forecasts, and it accounts for up to one fifth of the atmospheric error for GNSS measurements. Hence, mea-suring the amount of water vapor in the atmosphere is important. Previously, data from GNSS base stations has been used to compute tomographic estimates for the water vapor distribution. Here, we present a technique that enables doing these tomographic estimates with receivers residing at roving positions instead of ones with a pre-determined position. Specifically, we show that combining proba-bilistic precise point positioning (PPP) with Bayesian tomography with 1 Hz posteriori update rate leads to the convergence of both the receiver position estimates and the wet residual estimates. Moreover, our findings include the fact that even low quality receiver data, such as the one crowdsourced from consumer-level equipment such as smartphones, may be used to improve the water vapor estimate, if the uncertainty models are not too optimistic nor too pessimistic. Simulated GNSS observations with realistic errors for up to one thousand GNSS receivers in Southern France, presented in the antecedent work (De Oliveira Marques et al., 2020), are employed for elaborate testing. We discuss why the proposed method is likely straightforwardly applicable on data coming from moving modern multi-sensor systems, although our testing data is limited to receivers that are not moving. Applications for the proposed technique include benefits in regions that are not covered by high-quality weather measurement instruments, e.g. islands, seas, and other remote areas such as the Arctic.(c) 2022 COSPAR. Published by Elsevier B.V. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).

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