Rising Planetary Boundary Layer Height over the Sahara Desert and Arabian Peninsula in a Warming Climate

• Published in: Journal of climate Vol. 34; no. 10; pp. 4043 - 4068
• Main Authors: Zhou, Liming, Tian, Yuhong, Wei, Nan, Ho, Shu-peng, Li, Jing
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 01.05.2021
• Subjects: Aerodynamics; Atmosphere; Boundary layer height; Boundary layers; Climate; Climate change; Climate models; Confidence; Datasets; Deserts; Earth surface; Enthalpy; Free atmosphere; Gases; Global warming; Heat; Heat exchange; Height; Humidity; Latent heat; Moisture; Momentum; Planetary boundary layer; Radiosonde soundings; Radiosondes; Relative humidity; Sensible heat; Soundings; Surface temperature; Temperature; Trace gases; Trends; Turbulent mixing; Arabian Peninsula; Sahara Desert; India
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/JCLI-D-20-0645.1

Turbulent mixing in the planetary boundary layer (PBL) governs the vertical exchange of heat, moisture, momentum, trace gases, and aerosols in the surface–atmosphere interface. The PBL height (PBLH) represents the maximum height of the free atmosphere that is directly influenced by Earth’s surface. This study uses a multidata synthesis approach from an ensemble of multiple global datasets of radiosonde observations, reanalysis products, and climate model simulations to examine the spatial patterns of long-term PBLH trends over land between 60°S and 60°N for the period 1979–2019. By considering both the sign and statistical significance of trends, we identify large-scale regions where the change signal is robust and consistent to increase our confidence in the obtained results. Despite differences in the magnitude and sign of PBLH trends over many areas, all datasets reveal a consensus on increasing PBLH over the enormous and very dry Sahara Desert and Arabian Peninsula (SDAP) and declining PBLH in India. At the global scale, the changes in PBLH are significantly correlated positively with the changes in surface heating and negatively with the changes in surface moisture, consistent with theory and previous findings in the literature. The rising PBLH is in good agreement with increasing sensible heat and surface temperature and decreasing relative humidity over the SDAP associated with desert amplification, while the declining PBLH resonates well with increasing relative humidity and latent heat and decreasing sensible heat and surface warming in India. The PBLH changes agree with radiosonde soundings over the SDAP but cannot be validated over India due to lack of good-quality radiosonde observations.