Abstract
In this study, the characteristics of climate extremes are investigated in different climatic regions and different seasons over Saudi Arabia for the period 1978–2021. For this purpose, the climate extreme indices are calculated using two methods: (i) fixed threshold and (ii) the standard metrics defined by the Expert Team on Climate Change Detection and Indices (ETCCDI). The temperature and rainfall extremes are computed for five climatic regions within Saudi Arabia, namely northern, coastal, interior, highland, and southern. The indices measuring the occurrence of warm days reveal an increasing trend in all seasons and regions, with the highest increases in the highland and interior regions. Warm days occur most frequently in autumn, followed by winter. There is a decreasing trend in the occurrence of cold nights, with trend rates higher in the highland and northern regions. The decreasing trend in cold nights is observed mostly in the winter, spring, and autumn seasons. Rainfall, as well as the frequency of wet days and very wet days, is all increasing in the northern and southern regions — an indication of more flash floods in these regions. On the other hand, the frequency of wet and very wet days is decreasing in the interior and highland regions — an alarming sign for future drought events. The trends in the above indices are almost flat in the coastal region. Results indicate that wet season rainfall dominates in the northern, coastal, and interior regions, while dry season rainfall occurs mostly in the highland and southern regions. Such information on the regional and seasonal variations of climate extremes can be used by planners and decision-makers of the country.
Similar content being viewed by others
References
Almazroui M (2019) Climate extremes over the Arabian Peninsula using RegCM4 for present conditions forced by several CMIP5 models. Atmos 10(11):675. https://doi.org/10.3390/atmos10110675
Almazroui M (2020a) Changes in temperature trends and extremes over Saudi Arabia for the period 1978–2019. Adv Meteorol Article ID 8828421, 21. https://doi.org/10.1155/2020/8828421
Almazroui M (2020b) Summer maximum temperature over the gulf cooperation council states in the twenty-first century: multimodel simulations overview. Arab J Geosci 13:477. https://doi.org/10.1007/s12517-020-05537-x
Almazroui M (2020c) Rainfall trends and extremes in Saudi Arabia in recent decades. Atmos 11:964. https://doi.org/10.3390/atmos11090964
Almazroui M, Islam MN, Athar H et al (2012a) Recent climate change in the Arabian Peninsula: annual rainfall and temperature analysis of Saudi Arabia for 1978–2009. Int J Climatol 32(6):953–966
Almazroui M, Islam MN, Jones PD et al (2012b) Recent climate change in the Arabian Peninsula: seasonal rainfall and temperature climatology of Saudi Arabia for 1979–2009. Atmos Res 111:29–45
Almazroui M, Dambul R, Islam MN, Jones PD (2014a) Principal components-based regionalization of the Saudi Arabian climate. Int J Climatol 35(9):2555–2573. https://doi.org/10.1002/joc.413
Almazroui M, Islam MN, Dambul R, Jones PD (2014b) Trends of temperature extremes in Saudi Arabia. Int J Climatol 34(3):808–826. https://doi.org/10.1002/joc.3722
Almazroui M, Islam MN, Saeed S et al (2020) Future changes in climate over the Arabian Peninsula based on CMIP6 multimodel simulations. Earth Syst Environ 4:611–630. https://doi.org/10.1007/s41748-020-00183-5
Almazroui M, Kamil S, Ammar K et al (2016) Climatology of the 500-hPa Mediterranean storms associated with Saudi Arabia wet season precipitation. Clim Dyn 47:3029–3042. https://doi.org/10.1007/s00382-016-3011-0
Almazroui M, Saeed F, Saeed S et al (2021) Projected changes in climate extremes using CMIP6 simulations over SREX regions. Earth Syst Environ 5:481–497. https://doi.org/10.1007/s41748-021-00250-5
Atif RM, Siddiqui MH, Almazroui M (2020) Near-real-time spatiotemporal analysis of convection and extreme rainfall leading to a flash flood using MSG-SEVIRI and TRMM data: A case study of a flash flood in Jeddah. J Flood Risk Manag 13(3):e12611
Atifa RM, Almazroui M, Saeed S, Abid MA, Islam MN, Ismail M (2020) Extreme precipitation events over Saudi Arabia during the wet season and their associated teleconnections. Atmos Res 231:104655. https://doi.org/10.1016/j.atmosres.2019.104655
de Vries AJ, Tyrlis E, Edry D, Krichak SO, Steil B, Lelieveld J (2013) Extreme precipitation events in the Middle East: dynamics of the Active Red Sea Trough. J Geophys Res-Atmos 118(13):7087–7108
Donat MG, Peterson TC, Brunet M et al (2014) Changes in extreme temperature and precipitation in the Arab region: long-term trends and variability related to ENSO and NAO. Int J Climatol 34:581–592. https://doi.org/10.1002/joc.3707
Islam MN, Almazroui M, Dambul R et al (2014) Long-term changes in seasonal temperature extremes over Saudi Arabia during 1981–2010. Int J Climatol 35(7): 1579-1592. https://doi.org/10.1002/joc.413
Krishna VL (2014) Long term temperature trends in four different climatic zones of Saudi Arabia. Int J Appl Sci Technol 4(5):233–242
Saeed S, Almazroui M (2019) Impacts of mid-latitude circulation on winter precipitation over the Arabian Peninsula. Clim Dyn 53:5253–5264. https://doi.org/10.1007/s00382-019-04862-6
Saeed S, Kucharski F, Almazroui M (2022) Impacts of mid-latitude circulation on winter temperature variability in the Arabian Peninsula: the explicit role of NAO. Clim Dyn. https://doi.org/10.1007/s00382-022-06313-1
Salimi M, Al-Ghamdi SG (2020) Climate change impacts on critical urban infrastructure and urban resiliency strategies for the Middle East. Sustain Cities Soc 54, Article ID 101948, 2020
Sherwood SC, Huber M (2010). An adaptability limit to climate change due to heat stress. Massachusetts Institute of Technology, Cambridge, MA 107 (21): 9552-9555. https://doi.org/10.1073/pnas.0913352107
Stokes B, Wike R, Carle J (2015) Global concern about climate change, broad support for limiting emissions. Pew Research Center, 1615 L St. NW, Suite 800 Washington, DC 20036, USA. Available at https://www.pewresearch.org/global/2015/11/05/1-concern-about-climate-change-and-its-consequences/. Accessed in May 2022
Vohra A (2021) The Middle East is becoming literally uninhabitable. Available at https://foreignpolicy.com/2021/08/24/the-middle-east-is-becoming-literally-uninhabitable/. Accessed in May 2022
Zhang X, Yang F (2004) RClimDex Software 1.0. http://etccdi.pacificclimate.org/software.shtml
Zhang X, Alexander L, Hegerl GC et al (2011) Indices for monitoring changes in extremes based on daily temperature and precipitation data. Wiley Interdiscip Rev Clim Chang 2(6):851–870
Zittis G, Hadjinicolaou P, Almazroui M et al (2021) Business-as-usual will lead to super and ultra-extreme heatwaves in the Middle East and North Africa. npj Climate and Atmospheric. Science 4:20. https://doi.org/10.1038/s41612-021-00178-7
Zittis G, Almazroui M, Alpert P et al (2022) Climate change and weather extremes in the Eastern Mediterranean and Middle East. Rev Geophys 60:e2021RG000762. https://doi.org/10.1029/2021RG000762
Acknowledgements
The authors acknowledge the King Abdulaziz University for its support and the National Center for Meteorology for providing necessary data. Computation for the work described in this paper was performed using Aziz Supercomputer at King Abdulaziz University’s High-Performance Computing Center, Jeddah, Saudi Arabia.
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
Conflict of interest
The authors declare no competing interests.
Additional information
Responsible Editor: Biswajeet Pradhan
Rights and permissions
Springer Nature or its licensor holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
About this article
Cite this article
Almazroui, M., Halwani, H.A., Islam, M.N. et al. Regional and seasonal variation of climate extremes over Saudi Arabia: observed evidence for the period 1978–2021. Arab J Geosci 15, 1605 (2022). https://doi.org/10.1007/s12517-022-10882-0
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s12517-022-10882-0