Skip to main content

Advertisement

Log in

On the contribution of dynamic leaf area index in simulating the African climate using a regional climate model (RegCM4)

  • Original Paper
  • Published:
Theoretical and Applied Climatology Aims and scope Submit manuscript

Abstract

To understand the contribution of dynamic leaf area index (LAI) in simulating the surface African climate, two 12-year simulations were analysed. The first simulation operates in the satellite phenology (SP) mode; meanwhile the second simulation relies on activating the carbon-nitrogen (CN) module. Both simulations used the variable infiltration capacity (VIC) as a land-surface hydrology scheme. The first simulation was referred to as SP-VIC, and the second one was designated as CN-VIC. The results showed that CN-VIC severely decrease LAI more than the SP-VIC particularly over the Congo basin. This leads to a severe decrease in vegetative evaporation and transpiration and a pronounced increase of soil evaporation in comparison with the SP-VIC. As a result, a remarkable decrease of total evapotranspiration was observed leading to a high warm bias relative to an observational dataset. The rate of total precipitation was less than when it is simulated by the SP-VIC, due to a decrease in the amount of water vapour transferred to the atmosphere. To ensure a superior performance of the coupled CN-VIC system, the four surface parameters of the VIC all need to be recalibrated over Africa particularly over the Congo basin, so the vegetation status and surface climate of Africa can be properly simulated.

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

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6

Similar content being viewed by others

References

  • Alo A, Wang G (2010) Role of dynamic vegetation in regional climate predictions over western Africa. Clim Dyn 35:907–922. https://doi.org/10.1007/s00382-010-0744-z

    Article  Google Scholar 

  • Anwar SA, Zakey A, Robaa S et al (2019) The influence of two land-surface hydrology schemes on the regional climate of Africa using the RegCM4 model. Theor Appl Climatol 136:1535–1548. https://doi.org/10.1007/s00704-018-2556-8

    Article  Google Scholar 

  • Beck HE, Albert IJM, Levizzani V, Schellekens J, Miralles DG, Martens B, Roo A (2017) MSWEP: 3-hourly 0.25 global gridded precipitation (1979–2015) by merging gauge, satellite, and reanalysis data. Hydrol Earth Syst Sci https://doi.org/10.5194/hess-2016-236

  • Bonan GB (2016) Ecological Climatology: concepts and applications. National Center for Atmospheric Research, Boulder, Colorado – Third edition.

  • Dee DP, Uppala SM, Simmons AJ, Berrisford P, Poli P, Kobayashi S, Andrae U, Balmaseda MA, Balsamo G, Bauer P, Bechtold P, Beljaars ACM, van de Berg L, Bidlot J, Bormann N, Delsol C, Dragani R, Fuentes M, Geer AJ, Haimberger L, Healy SB, Hersbach H, Hólm EV, Isaksen L, Kållberg P, Köhler M, Matricardi M, McNally AP, Monge-Sanz BM, Morcrette JJ, Park BK, Peubey C, de Rosnay P, Tavolato C, Thépaut JN, Vitart F (2011) The ERA-interim reanalysis: configuration and performance of the data assimilation system. QJR Meteorol Soc 137:553–597

    Article  Google Scholar 

  • Emanuel KA (1991) A scheme for representing cumulus convection in large-scale models. J Atmos Sci 48(21):2313–2335

    Article  Google Scholar 

  • Erfanian A, Wang G, Yu M, Anyah R (2016) Multi-model ensemble simulations of present and future climates over West Africa: Impacts of vegetation dynamics. J Adv Model Earth Syst 8:1411–1431. https://doi.org/10.1002/2016MS000660

    Article  Google Scholar 

  • Fang Y, Liu C, Leung LR (2015) Accelerating the spin-up of the coupled carbon and nitrogen cycle model in CLM4. Geosci Model Dev 8:781–789

    Article  Google Scholar 

  • Grenier H, Bretherton CS (2001) A moist PBL parameterization for large-scale models and its application to subtropical cloud topped marine boundary layers. Mon Weather Rev 129:357–377

    Article  Google Scholar 

  • Harris I, Jones PD, Osborna TJ, Lister DH (2014) Updated high-resolution grids of monthly climatic observations – the CRU TS3.10 dataset. Int J Climatol 34:623–642

    Article  Google Scholar 

  • Huang M, Liang X (2006) On the assessment of the impact of reducing parameters and identification of parameter uncertainties for a hydrologic model with applications to ungauged basins. J Hydrol 320:37–61

    Article  Google Scholar 

  • Hu YX, Stamnes K (1993) An accurate parameterization of the radiative properties of water clouds suitable for use in climate models. J Clim 6:728–742

    Article  Google Scholar 

  • Jung M, Reichstein M, Bondeau A (2009) Towards global empirical upscaling of FLUXNET eddy covariance observations: validation of a model tree ensemble approach using a biosphere model. Biogeosciences 6:2001–2013

    Article  Google Scholar 

  • Jung M, Reichstein M, Margolis HA, Cescatti A et al (2011) Global patterns of land-atmosphere fluxes of carbon dioxide, latent heat, and sensible heat derived from eddy covariance, satellite, and meteorological observations. J Geophys Res 116:G00J07. https://doi.org/10.1029/2010JG001566

    Article  Google Scholar 

  • Kain JS (2003) The Kain–Fritsch convective parameterization: an update. J Appl Meteorol 43:170–181

    Article  Google Scholar 

  • Kanamitsu M, Ebisuzaki W, Woollen J, Yang SK, Hnilo JJ, Fiorino M, Potter GL (2002) NCEP-DOE AMIP-II reanalysis (R-2). Bull Am Meteorol Soc 83:1631–1643

    Article  Google Scholar 

  • Lei H, Huang M, Leung LR, Yang D, Shi X, Mao J, Hayes DJ, Schwalm CR, Wei Y, Liu S (2014) Sensitivity of global terrestrial gross primary production to hydrologic states simulated by the community land model using two runoff parameterizations. J Adv Model Earth Syst 6:658–679. https://doi.org/10.1002/2013MS000252

    Article  Google Scholar 

  • Manabe S (1969) Climate and the ocean circulation: 1, the atmospheric circulation and the hydrology of the Earth’s surface. Mon Weather Rev 97:739–805

    Article  Google Scholar 

  • Oleson KW, Lawrence DM (2013) Technical description of version 4.5 of the community land model (CLM). NCAR/TN-503+STR NCAR technical note

  • Prentice IC, Liang X, Medlyn BE, Wang YP (2015) Reliable, robust and realistic: the three R’s of next-generation land-surface modeling. Atmos Chem Phys 15:5987–6005

    Article  Google Scholar 

  • Sellers PJ, Randall DA, Collatz CJ, Berry JA, Field CB, Dazlich DA, Zhang C, Collelo G, Bounoua L (1996) A revised land-surface parameterization (SiB2) for atmospheric GCMs; part 1: model formulation. J Clim 9:676–705

    Article  Google Scholar 

  • Sellers PJ, Heiser MD, Hall FG, Verma SB, Desjardins RL, Schuepp PM, MacPherson JI (1997) The impact of using area-average land surface properties – topography, vegetation condition, soil wetness – in calculation of intermediate scale (approximately 10 km2 ) surface-atmosphere heat and moisture fluxes. J Hydrol 190:269–301

    Article  Google Scholar 

  • Thornton PE, Law BE, Gholz HL, Clark KL, Falge E, Ellsworth DS, Goldstein AH, Monson RK, Hollinger D, Falk M, Chen J, Sparks JP (2002) Modelling and measuring the effects of disturbance history and climate on carbon and water budgets in evergreen needleleaf forests. Agric For Meteorol 113:185–222

    Article  Google Scholar 

  • Thornton PE, Rosenbloom NA (2005) Ecosystem model spin-up: estimating steady state conditions in a coupled terrestrial carbon and nitrogen cycle model. Ecol Model 189:25–48

    Article  Google Scholar 

  • Thornton PE, Zimmermann NE (2007) An improved canopy integration scheme for a land surface model with prognostic canopy structure. J. Climate 20:3902–3923

    Article  Google Scholar 

  • Wang G, Yul M, Pal JS, Mei R, Bonan GB, Levis S, Thornton PE (2015) On the development of a coupled regional climate–vegetation model RCM–CLM–CN–DV and its validation in tropical Africa. Clim Dyn 46:515–539. https://doi.org/10.1007/s00382-015-2596-z

    Article  Google Scholar 

  • Wu M, Schurgers G, Rummukainen M, Smith B, Samuelsson P, Jansson C, Siltberg J, May W (2016) Vegetation–climate feedbacks modulate rainfall patterns in Africa under future climate change. Earth Syst Dynam 7:627–647. https://doi.org/10.5194/esd-7-627-2016

    Article  Google Scholar 

  • Yu M, Wang G, Pal JS (2015) Effects of vegetation feedback on future climate change over West Africa. Clim Dyn 46:3669–3688. https://doi.org/10.1007/s00382-015-2795-7

    Article  Google Scholar 

Download references

Acknowledgements

OFID-ICTP is acknowledged for supporting the fund for the step program in ICTP institute. The climate group in international centre for theoretical physics (ICTP)—Earth System Physics (ESP) team is acknowledged for providing the RegCM code, computational facilities, and input data to run the model. Climate Research Unit (CRU) of University of East Anglia is acknowledged for providing observed data set of mean temperature. We are grateful for Dr. Martin Jung for providing the up-scaled flux-net dataset of latent and sensible heat fluxes (MTE datasets) through BGI portal. NCEP Reanalysis data provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA, from their Web site at http://www.esrl.noaa.gov/psd/. Dr. Enda O’Brien (Climate Scientist— CECCR, King Abdul-Aziz University Jeddah; Saudi Arabia) is acknowledged for improving the quality of the manuscript.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Samy A. Anwar.

Additional information

Publisher’s note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Anwar, S.A. On the contribution of dynamic leaf area index in simulating the African climate using a regional climate model (RegCM4). Theor Appl Climatol 143, 119–129 (2021). https://doi.org/10.1007/s00704-020-03414-x

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00704-020-03414-x

Navigation