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The effects of boreal forest expansion on the summer Arctic frontal zone

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Abstract

Over the last 100 years, Arctic warming has resulted in a longer growing season in boreal and tundra ecosystems. This has contributed to a slow northward expansion of the boreal forest and a decrease in the surface albedo. Corresponding changes to the surface and atmospheric energy budgets have contributed to a broad region of warming over areas of boreal forest expansion. In addition, mesoscale and synoptic scale patterns have changed as a result of the excess energy at and near the surface. Previous studies have identified a relationship between the positioning of the boreal forest-tundra ecotone and the Arctic frontal zone in summer. This study examines the climate response to hypothetical boreal forest expansion and its influence on the summer Arctic frontal zone. Using the Weather Research and Forecasting model over the Northern Hemisphere, an experiment was performed to evaluate the atmospheric response to expansion of evergreen and deciduous boreal needleleaf forests into open shrubland along the northern boundary of the existing forest. Results show that the lower surface albedo with forest expansion leads to a local increase in net radiation and an average hemispheric warming of 0.6°C at and near the surface during June with some locations warming by 1–2°C. This warming contributes to changes in the meridional temperature gradient that enhances the Arctic frontal zone and strengthens the summertime jet. This experiment suggests that continued Northern Hemisphere high-latitude warming and boreal forest expansion might contribute to additional climate changes during the summer.

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References

  • ACIA (2004) Impact of a warming Arctic: Arctic climate impact assessment. Cambridge University Press, Cambridge, p 146

    Google Scholar 

  • Beringer J, Tapper NJ, McHugh I, Chapin FS III, Lynch AH, Serreze MC, Slater AG (2001) Impact of Arctic treeline on synoptic climate. Geophys Res Lett 28:4247–4250

    Article  Google Scholar 

  • Bhatt US, Walker DA, Raynolds MK, Comiso JC, Epstein HE, Jia G, Gens R, Pinzon JE, Tucker CJ, Tweedie CE, Webber PJ (2010) Circumpolar Arctic tundra vegetation change is linked to sea ice decline. Earth Interact 14:1–20

    Article  Google Scholar 

  • Bonan GB (2008) Forests and climate change: forcings, feedbacks, and the climate benefits of forests. Science 320:1444–1449

    Article  Google Scholar 

  • Bonan GB, Pollard D, Thompson SL (1992) Effects of boreal forest vegetation on global climate. Nature 359:716–718

    Article  Google Scholar 

  • Bonan GB, Chapin FSI, Thompson SL (1995) Boreal forest and tundra ecosystems as components of the climate system. Clim Change 29:145–167

    Article  Google Scholar 

  • Bromwich DH, Hines KM, Bai LS (2009) Development and testing of polar weather research and forecasting model: 2. Arctic Ocean. J Geophys Res 114:D08122

    Article  Google Scholar 

  • Bryson RA (1966) Air masses, streamlines, and the boreal forest. Geograph Bull 8:228–269

    Google Scholar 

  • Chang E (2009) Are band-pass variance statistics useful measures of storm track activity? Re-examining storm track variability associated with the NAO using multiple storm track measures. Clim Dyn 33:277–296

    Article  Google Scholar 

  • Chapin F, Sturm M, Serreze M, McFadden J, Key J, Lloyd A, McGuire A, Rupp T, Lynch A, Schimel J, Beringer J, Chapman W, Epstein H, Euskirchen E, Hinzman L, Jia G, Ping C, Tape K, Thompson C, Walker D, Welker J (2005) Role of land-surface changes in Arctic summer warming. Science 310:657–660

    Article  Google Scholar 

  • Chapin F, McGuire A, Ruess R, Hollingsworth T, Mack M, Johnstone J, Kasischke E, Euskirchen E, Jones J, Jorgenson M (2010) Resilience of Alaska’s boreal forest to climatic change. Can J For Res 40:1360–1370

    Article  Google Scholar 

  • Davis MB, Shaw RG (2001) Range shifts and adaptive responses to quaternary climate change. Science 292:673–679

    Article  Google Scholar 

  • De Haan LL, Kanamitsu M, Lu C-H, Roads JO (2007) A comparison of the Noah and OSU land surface models in the ECPC seasonal forecast model. J Hydrometeorol 8:1031–1048

    Article  Google Scholar 

  • Euskirchen ES, McGuire AD, Kicklighter DW, Zhuang Q, Clein JS, Dargaville RJ, Dye DG, Kimball JS, McDonald KC, Melillo JM, Romanovsky VE, Smith NV (2006) Importance of recent shifts in soil thermal dynamics on growing season length, productivity, and carbon sequestration in terrestrial high-latitude ecosystems. Glob Change Biol 12:731–750

    Article  Google Scholar 

  • Fischlin A, Midgley GF, Price J, Leemans R, Gopal B, Turley C, Rounsevell MDA, Dube P, Tarazona J, Velichko AA (2007) Ecosystems, their properties, goods and services. In: Parry ML, Canziani OF, Palutikof JP, van der Linden PJ, Hanson CE (eds) Climate change 2007: impacts, adaptation and vulnerability contribution of working group II to the fourth assessment report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, pp 211–272

    Google Scholar 

  • Foley JA, Kutzbach JE, Coe MT, Levis S (1994) Feedbacks between climate and boreal forests during the Holocene epoch. Nature 371:52–54

    Article  Google Scholar 

  • Foley JA, Prentice IC, Ramankutty N, Levis S, Pollard D, Sitch S, Haxeltine A (1996) An integrated biosphere model of land surface processes, terrestrial carbon balance, and vegetation dynamics. Global Biogeochem Cycles 10:603–628

    Article  Google Scholar 

  • Gamache I, Payette S (2005) Latitudinal response of subarctic tree lines to recent climate change in eastern Canada. J Biogeogr 32:849–862

    Article  Google Scholar 

  • Hare FK, Ritchie JC (1972) The boreal bioclimates. Geogr Rev 62:333–365

    Article  Google Scholar 

  • Harnik N, Chang EKM (2003) Storm track variations as seen in radiosonde observations and reanalysis data. J Clim 16:480–495

    Article  Google Scholar 

  • Higgins PAT, Harte J (2006) Biophysical and biogeochemical responses to climate change depend on dispersal and migration. Bioscience 56:407–417

    Article  Google Scholar 

  • Hines KM, Bromwich DH, Bai L-S, Barlage M, Slater AG (2011) Development and testing of polar WRF. Part III: Arctic land. J Clim 24:26–48

    Article  Google Scholar 

  • Jeong S-J, Ho C-H, Park T-W, Kim J, Levis S (2010) Impact of vegetation feedback on the temperature and its diurnal range over the Northern Hemisphere during summer in a 2 × CO2 climate. Clim Dyn. doi: 10.1007/s00382-010-0827-x

  • Jia G, Epstein HE, Walker DA (2003) Greening of arctic Alaska, 1981–2001. Geophys Res Lett 30:1029–1033

    Article  Google Scholar 

  • Kain JS (2004) The Kain–Fritsch convective parameterization: an update. J Appl Meteorol 43:170–181

    Article  Google Scholar 

  • Kain JS, Fritsch JM (1990) A one-dimensional entraining-detraining plume model and its application in convective parameterization. J Atmos Sci 47:2784–2802

    Article  Google Scholar 

  • Kain JS, Fritsch JM (1993) Convective parameterization for mesoscale models: the Kain–Fritsch scheme. The representation of cumulus convection in numerical models. Meteorol Monogr 24:165–170

    Google Scholar 

  • Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woollen J, Zhu Y, Chelliah M, Ebisuzaki W, Higgins W, Janowiak J, Mo KC, Ropelewski C, Wang J, Leetmaa A, Reynolds R, Jenne R, Joseph D (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteorol Soc 77:437–471

    Article  Google Scholar 

  • Koren V, Schaake J, Mitchell K, Duan QY, Chen F, Baker JM (1999) A parameterization of snowpack and frozen ground intended for NCEP weather and climate models. J Geophys Res 104:19569–19585

    Article  Google Scholar 

  • Krebs JS, Barry RG (1970) The Arctic front and the Tundra–Taiga boundary in Eurasia. Geogr Rev 60:548–554

    Article  Google Scholar 

  • Kurz WA, Dymond CC, Stinson G, Rampley GJ, Neilson ET, Carroll AL, Ebata T, Safranyik L (2008) Mountain pine beetle and forest carbon feedback to climate change. Nature 452:987–990

    Article  Google Scholar 

  • Levis S, Foley JA, Brovkin V, Pollard D (1999a) On the stability of the high-latitude climate-vegetation system in a coupled atmosphere-biosphere model. Glob Ecol Biogeogr 8:489–500

    Article  Google Scholar 

  • Levis S, Foley JA, Pollard D (1999b) Potential high-latitude vegetation feedbacks on CO2-induced climate change. Geophys Res Lett 26:747–750

    Article  Google Scholar 

  • Levis S, Foley JA, Pollard D (2000) Large-scale vegetation feedbacks on a doubled CO2 climate. J Clim 13:1313–1325

    Article  Google Scholar 

  • Lynch A, Slater A, Serreze M (2001) The Alaskan Arctic frontal zone: forcing by orography, coastal contrast, and the boreal forest. J Clim 14:4351–4362

    Article  Google Scholar 

  • Meehl GA, Stocke TF, Collins WD, Friedlingstein P, Gaye AT, Gregory JM, Kitoh A, Knutti R, Murphy JM, Noda A, Raper SCB, Watterson IG, Weaver AJ, Zhao Z-C (2007) Global 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, pp 747–846

    Google Scholar 

  • Morrison H, Thompson G, Tatarskii V (2009) Impact of cloud microphysics on the development of trailing stratiform precipitation in a simulated squall line: comparison of one- and two-moment schemes. Mon Weather Rev 137:991–1007

    Article  Google Scholar 

  • Myneni RB, Keeling CD, Tucker CJ, Asrar G, Nemani RR (1997) Increased plant growth in the northern hight latitudes from 1981 to 1991. Nature 386:698–702

    Article  Google Scholar 

  • Overpeck J, Hughen K, Hardy D, Bradley R, Case R, Douglas M, Finney B, Gajewski K, Jacoby G, Jennings A, Lamoureux S, Lasca A, MacDonald G, Moore J, Retelle M, Smith S, Wolfe A, Zielinski G (1997) Arctic environmental change of the last four centuries. Science 278:1251–1256

    Article  Google Scholar 

  • Pielke RA, Vidale PL (1995) The boreal forest and the polar front. J Geophys Res 100:25755–25758

    Article  Google Scholar 

  • Reed RJ, Kunkel BA (1960) The Arctic circulation in summer. J Meteorol 17:489–506

    Article  Google Scholar 

  • Sellers P, Hall F, Margolis H, Kelly B, Baldocchi D, Denhartog G, Cihlar J, Ryan MG, Goodison B, Crill P, Ranson KJ, Lettenmaier D, Wickland DE (1995) The boreal ecosystem-atmosphere study (Boreas)—an overview and early results from the 1994 field year. Bull Am Meteorol Soc 76:1549–1577

    Article  Google Scholar 

  • Serreze MC, Key JR, Box JE, Maslanik JA, Steffen K (1998) A new monthly climatology of global radiation for the Arctic and comparisons with NCEP-NCAR reanalysis and ISCCP-C2 fields. J Clim 11:121–136

    Article  Google Scholar 

  • Serreze M, Lynch A, Clark M (2001) The Arctic frontal zone as seen in the NCEP-NCAR reanalysis. J Clim 14:1550–1567

    Article  Google Scholar 

  • Skamarock WC, Klemp JB, Dudhia J, Gill DO, Barker DM, Duda MG, Huang X-Y, Wang W, Powers JG (2008) A description of the advanced research WRF version 3. NCAR technical note 475. National Center for Atmospheric Research, Boulder, p 125

    Google Scholar 

  • Snyder P, Delire C, Foley J (2004) Evaluating the influence of different vegetation biomes on the global climate. Clim Dyn 23:279–302

    Article  Google Scholar 

  • Sridhar V, Elliott RL, Chen F, Brotzge JA (2002) Validation of the NOAH-OSU land surface model using surface flux measurements in Oklahoma. J Geophys Res 107:4418

    Article  Google Scholar 

  • Sturm M, Racine C, Tape K (2001) Climate change—increasing shrub abundance in the Arctic. Nature 411:546–547

    Article  Google Scholar 

  • Tape K, Sturm M, Racine C (2006) The evidence for shrub expansion in Northern Alaska and the Pan-Arctic. Glob Change Biol 12:686–702

    Article  Google Scholar 

  • Trenberth KE, Jones PD, Ambenje P, Bojariu R, Easterling D, Klein Tank A, Parker D, Rahimzadeh F, Renwick JA, Rusticucci M, Soden B, Zhai P (2007) Observations: surface and atmospheric climate change. 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, pp 235–336

    Google Scholar 

  • Tucker CJ, Slayback DA, Pinzon JE, Los SO, Myneni RB, Taylor MG (2001) Higher northern latitude normalized difference vegetation index and growing season trends from 1982 to 1999. Int J Biometeorol 45:184–190

    Article  Google Scholar 

  • Wilks DS (2006) Statistical methods in the atmospheric sciences, 2nd edn. International geophysics series, 91. Academic Press, New York, p 465

    Google Scholar 

  • Zhang X, Friedl MA, Schaaf CB (2006) Global vegetation phenology from moderate resolution imaging spectroradiometer (MODIS): evaluation of global patterns and comparison with in situ measurements. J Geophys Res 111:G04017

    Article  Google Scholar 

  • Zhou LM, Tucker CJ, Kaufmann RK, Slayback D, Shabanov NV, Myneni RB (2001) Variations in northern vegetation activity inferred from satellite data of vegetation index during 1981 to 1999. J Geophys Res 106:20069–20083

    Article  Google Scholar 

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Acknowledgments

This study and the material herein are based upon work supported by the U.S. National Science Foundation under Grant No. ATM-0840048. This work was carried out in part using computing resources at the University of Minnesota Supercomputing Institute. The authors are indebted to two anonymous reviewers for their constructive comments on this manuscript.

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Correspondence to Stefan Liess.

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Liess, S., Snyder, P.K. & Harding, K.J. The effects of boreal forest expansion on the summer Arctic frontal zone. Clim Dyn 38, 1805–1827 (2012). https://doi.org/10.1007/s00382-011-1064-7

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