GNSS radio occultation in-filling of the African radiosonde data gaps reveals drivers of tropopause climate variability

Radiosonde data are important for understanding and monitoring the upper troposphere and lower stratosphere (UTLS) region. Over much of Africa, however, such data are lacking; consequently, the African UTLS is understudied, and potential proxies such as climate models and reanalysis products fail to...

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Bibliographic Details
Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Ding, Tong, Awange, Joseph, Scherllin-Pirscher, Barbara, Kuhn, Michael, Nakhap, Khandu, Anyah, Richard, Zerihun, Ayalsew, Luyen, Bui Khac
Other Authors: Randel, William
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2022
Subjects:
Science & Technology
Physical Sciences
Meteorology & Atmospheric Sciences
Africa
global and regional climate drivers
GNSS Radio Occultation
radiosonde
reanalyses
tropopause variability
INDEPENDENT COMPONENT ANALYSIS
NINO-SOUTHERN-OSCILLATION
TROPICAL TROPOPAUSE
GLOBAL RADIOSONDE
ATMOSPHERIC PROFILES
LOWER STRATOSPHERE
VAISALA RS80
ANNULAR MODE
TEMPERATURE
WATER
Indian
Merra
North Atlantic
North Atlantic oscillation
Online Access:https://hdl.handle.net/20.500.11937/91903
https://doi.org/10.1029/2022JD036648
Description
Summary:Radiosonde data are important for understanding and monitoring the upper troposphere and lower stratosphere (UTLS) region. Over much of Africa, however, such data are lacking; consequently, the African UTLS is understudied, and potential proxies such as climate models and reanalysis products fail to fully capture the behavior of the UTLS. This study pioneers the use of Global Navigation Satellite System-Radio Occultation (GNSS-RO) data from 2001 to 2020 to address the radiosonde data gap over Africa and contributes to a better understanding of the tropopause (TP) characteristics under the influence of global and regional climate drivers over the continent. As a first step to using GNSS-RO for infilling the radiosonde data gap over Africa, we analyzed the performance of GNSS-RO (2001–2020) and reanalysis products (European Centre for Medium-Range Weather Forecasts Reanalysis 5 (ERA5) and Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2)) against radiosonde observations applying the Kling-Gupta Efficiency metric. The analyses show that GNSS-RO data from Challenging Mini-satellite Payload, Gravity Recovery and Climate Experiment, Meteorological Operational, Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC), and COSMIC-2 are in good agreement with radiosonde measurements with differences being smaller than 1 K in the UTLS, thereby enabling infilling of missing radiosonde data in Africa during 2001–2020. By contrast, the smoothed vertical temperature profiles of reanalysis products lead to a warm bias of +0.8 K in ERA5 and +1.2 K in MERRA-2 and these biases alter some vertical and temporal structure details, with possible implications on climate change detection and attribution. Furthermore, the analysis of GNSS-RO data over Africa revealed: (a) the teleconnections of El Niño-Southern Oscillation (ENSO), Quasi-Biennial Oscillation (QBO), Indian Ocean Dipole (IOD), Madden-Julian Oscillation (MJO), North Atlantic Oscillation (NAO) and Southern Annular ...

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