Abstract

The data of GPS measurements at the permanent observation points IRKM (Irkutsk, 52°13′ N, 104°19′ E, h = 509 m), ULAZ (Ulan-Ude, 51°48′ N, 107°37′ E, h = 517 m) and BADG (Badary, 51°46′ N, 102°14′ E, h = 848 m) located within the Baikal natural area (Eastern Siberia) are considered. A comparison was made of the time series of the tropospheric moisture content levels obtained at the IRKM site from GPS observations and radiosonde data, and at the BADG site from GPS observations and measurements with a water vapor radiometer (WVR) during 2020. The average deviation of the difference in total moisture content data during 2020 in the form of precipitable water according to GPS and WVR observations was about 0.12 mm, or about 1.1% relative to the average value, and the cross-correlation coefficient between the data is very high (K = 0.92). The use of GPS observations to obtain continuous data on the moisture content of the troposphere is substantiated. A series of processed data on the total moisture content based on GPS measurements using surface meteorological data for the period 1999–2020 for the IRKM and ULAZ sites and for the period 2006–2020 for the BADG site were obtained. Linear trends of total moisture content were determined for observation points: IRKM (−0.35 mm per decade, –2.7%), ULAZ (+0.47 mm per decade, +3.9%) and BADG (+1.41 mm per decade, 13.4%). Moreover, at the IRKM and ULAZ points, the surface temperature trends in the same period were positive and amounted to +0.4 K and +0.7 K per decade, respectively. The article confirms the trends identified in the work of Ross and Elliott for the territory of Eastern Siberia.

Highlights

  • At present, a network of permanent GPS observations continues to be created within the Baikal natural territory

  • At points IRKM and BADG, a comparison of the values of the total moisture content of the atmosphere by the methods of radiosondes and water vapor radiometer (WVR) measurements with the method of GPS observations was carried out

  • The coefficient of cross-correlation between the measurement data of the WVR and GPS observations is equal to 0.92, and the average deviation of the difference is equal to 0.12 mm

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Summary

Introduction

A network of permanent GPS observations continues to be created within the Baikal natural territory. GPS observations are carried out for continuous monitoring of geodynamic processes in the seismically active Baikal rift zone [1]. GPS measurements allow for continuously obtaining data on the zenith tropospheric delay (ZTD) [2]. The total moisture content in the form of water vapor in the conventional vertical column is mainly determined in the troposphere. The reliability of the results of determining the total moisture content from GPS observations can be determined by comparing them with measurements by a microwave water vapor radiometer, which is the most accurate method for determining IWV, as well as with the results of radiosonde launches. GPS observations cannot provide a humidity profile as radiosondes do, but they have the advantage of providing continuous data whereas radiosondes provide only two or four measurements per day

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