EGU2020-10138
https://doi.org/10.5194/egusphere-egu2020-10138
EGU General Assembly 2020
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Diurnal cycle of GNSS-derived precipitable water vapour in tropical regions

Zofia Bałdysz1, Grzegorz Nykiel1,2, Dariusz Baranowski3, Beata Latos3, and Mariusz Figurski1,2
Zofia Bałdysz et al.
  • 1Faculty of Civil and Environmental Engineering, Gdansk University of Technology, Gdansk, Poland (zofia.baldysz@pg.edu.pl)
  • 2Institute of Meteorology and Water Management - National Research Institute, Warsaw, Poland
  • 3Institute of Geophysics Polish Academy of Sciences, Warsaw, Poland

Convective processes in the tropical atmosphere and their diurnal cycles have important repercussions for the circulations in the tropical regions and beyond. Monitoring of the water vapour content in the tropical atmosphere remains a challenge due to its high temporal and spatial variability. Global models tend to fail to correctly capture the diurnal convection, limiting forecasting accuracy. In this work, we investigated precipitable water vapour (PWV) diurnal cycle, precipitation and infrared  brightness temperature (TB) data over the tropical area. We used in-situ observations from 44 IGS (International GNSS Service) stations covering time span of 18 years, together with satellite-based precipitation and cloudiness data, taken from the Tropical Rainfall Measurement Mission gridded dataset (TRMM 3B42 v7) and the global, merged infrared (IR) dataset, respectively. The data provided an opportunity to examine the characteristics of a diurnal cycle of PWV, precipitation and TB over the study area in greater detail than before.

In particular, our results show that the diurnal cycle of PWV and TB were almost entirely dominated by mono-modal distributions. The diurnal cycle of precipitation onshore (continental areas or big islands; continental regime) had a single late afternoon peak, and that offshore (small islands; oceanic regime) had both a midday and a nocturnal peak. Daily amplitude phase shift of PWV and precipitation at onshore stations with a continental regime consistently occurred at the same time, while TB maximum peaked about five hours later. Furthermore, results show that the daily mean and the amplitude of the diurnal cycle of PWV, precipitation and TB appeared smaller on offshore stations, exhibited to an oceanic regime, than on onshore, continental stations. Additional analysis of seasonal variations of GNSS-derived PWV shows the usefulness of such measurements for tracking propagation of longer-scale phenomena, such as Inter Tropical Convergence Zone (ITCZ), Southeast Asian monsoon or East Asian summer monsoon.

How to cite: Bałdysz, Z., Nykiel, G., Baranowski, D., Latos, B., and Figurski, M.: Diurnal cycle of GNSS-derived precipitable water vapour in tropical regions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10138, https://doi.org/10.5194/egusphere-egu2020-10138, 2020