Skip to main content

Climate Change and Locusts in the WANA Region

  • Chapter
  • First Online:
Climate Change and Food Security in West Asia and North Africa

Abstract

The Desert Locust is probably the oldest and most feared migratory pest in the world, plaguing farmers in Africa and Asia since Phaoronic times. Under optimal conditions, locusts increase rapidly and form swarms. A single swarm, larger than Paris or Cairo, can contain billions of insects, migrate across continents, and eat enough food for 2,500 people in 1 day. During plagues, vulnerable households can find themselves in debt, limited national resources are rapidly depleted and food security can be at risk in affected countries. It can take several years and hundreds of millions of dollars to bring a plague to an end. Changes in the climate during the remainder of this century will affect Desert Locust habitats, breeding, migration and plague dynamics in West Asia and North Africa (WANA). Although it is widely acknowledged that WANA will become warmer, there are differing views about changes in precipitation under the various climate change scenarios. General trends may contain hidden variations within the regions and countries. Certain areas will become more prone to extreme events such as flooding and droughts. Regular assessment of climate change impacts is a component of the locust early warning system operated by the Food and Agriculture Organization (FAO) of the United Nations to monitor the global situation and alert locust-affected countries and international donors. The latest scientific evidence is reviewed to postulate potential effects on the Desert Locust. It is probably reasonable to assume that this ancient pest, which is particularly well suited for survival under difficult conditions in arid areas and has successfully endured previous changes in the climate, will adapt to climate variability in the foreseeable future.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 129.00
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 169.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 169.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Notes

  1. 1.

    The B1 scenario is one of an integrated world that is more ecological friendly, characterized by rapid economic growth, rising population to 2050 then declining, reductions in material intensity and the introduction of efficient technologies, and an emphasis on global solutions to economic, social and environmental stability.

  2. 2.

    The A2 scenario is of a more divided world characterized by independent operating, self-reliant nations, continuously increasing population, regionally oriented economic development, and slower technological changes and improvement to per capita income.

  3. 3.

    The main characteristics of the A1B scenario include low population growth, very high GDP growth, very high energy use, low-medium land use changes, medium resource (mainly oil and gas) availability, and rapid pace and direction of technological change favoring balanced development.

References

  • Biasutti M, Sobel AH, Camargo SJ (2009) The role of the Sahara low in summertime Sahel rainfall variability and change in the CMIP3 model. J Climate 22:5755–5771. doi:10.1175/2009JCLI29969.1

    Article  Google Scholar 

  • Christensen JH, Hewitson B, Busuioc A, Chen A, Gao X, Held I, Jones R, Kolli RK, Kwon WT, Laprise R, Magaña Rueda V, Mearns L, Menéndez CG, Räisänen J, Rinke A, Sarr A, Whetton P (2007) Regional climate projections. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Climate change 2007: the physical science basis. Contribution of working group I to the fourth assessment report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK

    Google Scholar 

  • Claussen M, Brovkin V, Ganopolski A, Kubatzki C, Petoukhov V (2003) Climate change in Northern Africa: the past is not the future. Clim Change 57:99–118

    Article  CAS  Google Scholar 

  • de Boer B (2007) The impact of climate change on rainfall extremes over Northeast Africa. Royal Netherlands Meteorological Institute (KNMI). De Bilt (The Netherlands), 46 pp

    Google Scholar 

  • Haarsma RJ, Selten F, Weber S, Kliphuis M (2005) Sahel rainfall variability and response to greenhouse warming. Geophys Res Lett 32:L17702. doi:10.1029/2005GL023232

    Article  Google Scholar 

  • Harley CDG, Randall Hughes A, Hultgren KM, Miner BG, Sorte CJB, Thornber CS, Rodriguez LF, Tomanek L, Williams SL (2006) The impacts of climate change in coastal marine systems. Ecol Lett 9:228–241. doi:10.1111/j.1461-0248.2005.00871.x

    Article  PubMed  Google Scholar 

  • Hulme M, Doherty R, Ngara T, New M, Lister D (2001) African climate change: 1900–2100. Clim Res 17:145–168

    Article  Google Scholar 

  • Pryor SC, Barthelmie RJ (2010) Climate change impacts on wind energy: a review. Renew Sust Energy Rev 14:430–437

    Article  Google Scholar 

  • Ren D (2010) Effects of global warming on wind energy availability. Renew Sust Energy Rev 2:052301. doi:10.1063/1.3486072

    Article  Google Scholar 

  • Reus JAWA, Symmons P (1992) A model to predict the incubation and nymphal development periods of the desert locust, Schistocerca gregaria (Orthoptera: Acrididae). Bull Entomol Res 82:517–520

    Article  Google Scholar 

  • Ritchie M, Pedgley D (1989) Desert Locust across the Atlantic. Antenna 13:10–12

    Google Scholar 

  • Schepanski K, Knippertz P (2011) Soudano-Saharan depressions and their importance for precipitation and dust: a new perspective on a classical synoptic concept. Q J Roy Meteor Soc 137:1431–1445. doi:10.1002/qj.850

    Article  Google Scholar 

  • Steedman A (ed) (1990) Locust handbook. Natural Resources Institute, Chatham, p 204

    Google Scholar 

  • Symmons P, Cressman K (2001) Desert locust guidelines I. Biology and behaviour. FAO, Rome, p 43

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Keith Cressman .

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2013 Springer Science+Business Media Dordrecht

About this chapter

Cite this chapter

Cressman, K. (2013). Climate Change and Locusts in the WANA Region. In: Sivakumar, M., Lal, R., Selvaraju, R., Hamdan, I. (eds) Climate Change and Food Security in West Asia and North Africa. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-6751-5_7

Download citation

Publish with us

Policies and ethics