Buradasınız

Projected Changes in Annual Temperature and Precipitation in Setif High Plains Region (North East of Algeria)

Journal Name:

Publication Year:

Abstract (2. Language): 
Known for its arid and semi-arid climate, Algeria is highly vulnerable to climate change. In this paper we present the projected temperature and precipitation changes in Setif high plains region (North East of Algeria) between three time slices: 2011- 2040 (centered on 2025), 2036-2065 (centered on 2050) and 2061-2090 (centered on 2075). MAGICC – SCENGEN5.3 (version 2) was used as a tool for downscaling the 4 chosen general circulation models (GCMs) output data. The projections are based on the SRES A2 and B2 scenarios. Under A2 scenario, The average model prediction of warming is 0.97, 1.75 and 2.88 °C across the three time slices, while the annual precipitation total is expected to reduce from -9% to -25.6%. Under B2 scenario, the four models estimate an increase in global temperature, but less than the first scenario. The average model prediction for the decrease in precipitation is -9%, -19.1% and -25.6% across the three periods.
FULL TEXT (PDF): 
45-48

REFERENCES

References: 

[1] H. Paeth, K. Born, R.Girmes, R. Podzun and D. Jacob, Regional climate change in Tropical and Northern Africa due to greenhouse forcing and land use changes, Bull. Amer. Meteor. Soc., vol 22, pp.114-132, 2009.
[2] J. Schilling K. Freier E. Hertig and J. Scheffran, Climate change, vulnerability and adaptation in North Africa with focus on Morocco, Working paper CLISEC-13, Research group climate change and security, University of Hamburg, 2011, 42pp.
[3] Caritas Internationalis, Climate change in Algeria, Climate Justice Newsletter, vol. 6, p.1, July 2011.
[4] T. M. L. Wigley, MAGICC/SCENGEN 5.3: User Manual (version 2), National center for atmospheric research (NCAR), Boulder, 2008, 80 pp.
[5] S.C.B. Raper, R.A. Warrick and T.M.L. Wigley, Global sea level rise: past and future. pp.11-45, 1996, In (Hulme M., Wigley T. M. L., Barrow E. M., Raper S. C. B., Centella A., Smith S. J and Chipanshi A. C., Using a climate scenario generator for vulnerability and adaptation assessments: MAGICC and SCENGEN Version 2.4Workbook, Climatic Research Unit. Norwich, United Kingdom, 2000, 52 pp.
[6] M. Hulme, T. M. L. Wigley, E. M. Barrow, S. C. B. Raper, A. Centella, S. J. Smith and A. C. Chipanshi, Using a climate scenario generator for vulnerability and adaptation assessments: MAGICC and SCENGEN version 2.4 Workbook. Climatic research unit, Norwich, United Kingdom. 52 pp. 2000.
[7] N. Nakićenović, and R. Swart, Special report on emissions scenarios, Cambridge University press, Cambridge, UK, 2000, 570 pp.
[8] C. Giannakopoulos, M. Bindi, M. Moriondo, P. Le Sager and T. Tin, Climate change impacts in the Mediterranean resulting from a 2°C global temperature rise, WWF Report, pp. 1-66, 2005.
[9] M. Bindi and M. Moriondo, Impact of a 2°C global temperature rise on the Mediterranean region: Agriculture analysis assessment, WWF Report, pp. 54-66, 2005.
[10] M.A. Malebajoa, Climate change impacts on crop yields and adaptive measures for agricultural sector in the lowlands of Lesotho, Master thesis, Lund University, Sweden, 2010, 55pp.
[11] C. Conde, F. Estrada, B. Martinez, O. Sanchez and C. Gay, Regional climate change scenarios for México, Atmósfera, vol. 24(1), pp. 125-140, 2011.
[12] F. Abbasi, M. Asmari and H. Arabshahi, Climate change assessment over Iran during future decades by using MAGICC-SCENGEN model, International Journal of Science and Advanced Technology, vol.1(5), p.89, July 2011.
[13] M. Hulme, R. Doherty, T. Ngara, M. New and D. Lister, African Climate Change: 1900-2100, Climate Research, p.14, 2000.
[14] IPCC., Bilan 2007 des changements climatiques. Contribution des Groupes de travail I, II et III au quatrième rapport d’évaluation du Groupe d’experts intergouvernemental sur l’évolution du climat. Genève, Suisse, 2007, 103pp.

Thank you for copying data from http://www.arastirmax.com