Abstract
Most dendrochronological studies are based on the relationship between total radial growth and precipitation; however, very few studies have considered the responses of early (EW) and late (LW) wood growth or the role of evaporation. In this study, residual indices for forests in the state of Durango (Mexico) during the period 1964-2010 were used to evaluate the response of EW and LW growth in Pinus cooperi Blanco to evaporation. DENDROCLIM software was used to correlate dendrochronological data to total monthly evaporation. Evaporation from January of the previous year to December of the current year was considered in a simple interval analysis. The coefficients of correlation indicated a consistent negative relationship between both EW and LW growth and evaporation in the fall/winter prior to the growth season. Nevertheless, LW growth was more consistent in terms of climatic sensitivity, which may indicate that measurement of this parameter may be more useful in dendroclimatic studies.
References
Biondi, F., & Waikul, K. (2004). DENDROCLIM2002: A C++ program for statistical calibration of climate signals in tree-ring chronologies. Computers & Geosciences, 30, 303–311. doi: https://doi.org/10.1016/j.cageo.2003.11.004
Cerano-Paredes, J., Méndez-González, J., Amaro-Sánchez, A., Villanueva-Díaz, J., Cervantes-Martínez, R., & Rubio-Camacho, E. A. (2013). Reconstrucción de precipitación invierno-primavera con anillos anuales de Pinus douglasiana en la Reserva de la Biosfera Sierra de Manantlán, Jalisco. Revista Chapingo Serie Ciencias Forestales y del Ambiente, 19(3), 413–423. doi: https://doi.org/10.5154/r.rchscfa.2013.02.007
Comisión Nacional del Agua (CONAGUA). (2012). Consultado 15-04-201 http://smn.cna.gob.mx/emas/
Cook, E. R., & Holmes, R. H. (1984). Program ARSTAN user manual. Tucson, AZ, USA: University of Arizona Press.
Cruz-Cobos, F., De los Santos-Posadas, H. M., & Valdez-Lazalde, J. R. (2008). Sistema compatible de ahusamiento-volumen para Pinus cooperi Blanco en Durango, México. Agrociencia, 42, 473–485. http://www.scielo.org.mx/pdf/agro/v42n4/v42n4a10.pdf
Díaz, S. C., Therrell, M. D., Stahle D. W., & Cleaveland, M. K. (2002). Chihuahua (Mexico) winter-spring precipitation reconstructed from tree-rings 1647-1992. Climate Research, 22, 237–244. http://www.intres.com/articles/cr2002/22/c022p237.pdf
Gochis, D. J., Brito-Castillo, L., & Shuttleworth, W. J. (2006). Hydroclimatology of the North American Monsoon region in northwest Mexico. Journal of Hydrology, 316, 53–70. http://www.cpc.ncep.noaa.gov/products/outreach/proceedings/cdw29_proceedings/Gochis.pdf
González-Elizondo, M. S., González-Elizondo, M., & Márquez, M. A. (2007). Vegetación y ecorregiones de Durango. México: Plaza y Valdés.
Griffin, D., Meko, D. M., Touchan, R., Leavitt, S. W., & Woodhouse, C. A. (2011). Latewood chronology development for summer-moisture reconstruction in the U. S. Southwest. Tree-Ring Research, 67(2), 87–101. doi: https://doi.org/10.3959/2011-4.1
Griffin, D., Woodhouse, C. A., Meko, D. M., Stahle, D. W., Faulstich, H. L., Carrillo, C, Leavitt, S. W. (2013). North American monsoon precipitation reconstructed from tree–ring latewood. Geophysical Research Letters, 40(5), 1–5. doi: https://doi.org/10.1002/grl.50184
Holmes, R. L. (1983). Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bulletin, 43, 69–78. http://arizona.openrepository.com/arizona/bitstream/10150/261223/1/trb-43-069-078.pdf
Liang, E. Y., Eckstein, D., Liu, H. Y. (2008). Climate-growth relationships of relict Pinus tabulaeformis at the northern limit of its natural distribution in northern China. Journal of Vegetation Science, 19, 393–406. doi: https://doi.org/10.3170/2008-8-18379
Meko, D. M., Touchan, R., Villanueva-Díaz, J., Griffin, D., Woodhouse, C. A., Castro, C. L, Leavitt, S. W. (2013). Sierra San Pedro Mártir, Baja California, cool-season precipitation reconstructed from earlywood width of Abies concolor tree rings. Journal of Geophysical Research: Biogeosciences,118,1660–1673 doi: https://doi.org/10.1002/2013JG002408
Mérian, P., Pierrat, J. C., & Lebourgeois, F. (2013). Effect of sampling effort on the regional chronology statistics and climate-growth relationships estimation. Dendrochronologia, 31, 58–67. doi: https://doi.org/10.1016/j.dendro.2012.07.001
Pompa-García, M., & Jurado, E. (2013). Seasonal precipitation reconstruction and teleconnections with ENSO based on tree ring analysis of Pinus cooperi. Theoretical and Applied Climatology. doi: https://doi.org/10.1007/s00704–013–1018–6
Pompa-García, M., Rodríguez-Flores, F. J., Aguirre-Salado, C. A., & Miranda-Aragón, L. (2013). Effect of evaporation on forest growth. Agrociencia, 47, 829–836. http://scielo.unam.mx/pdf/agro/v47n8/v47n8a7.pdf
Stahle, D. W., Villanueva-Diaz, J., Burnette, D. J., Cerano-Paredes, J., Heim, J. R. R., Fye, F. K., ...Stahle, D. K. (2011). Major Mesoamerican droughts of the past millennium. Geophysical Research Letters. doi: https://doi.org/10.1029/2010GL046472
Stokes, M. A., & Smiley, T. L. (1996). An introduction to tree-ring dating. Tucson, AZ, USA: University of Arizona Press.
Woodhouse, C. A., & Lukas, J. J. (2006). Multi-century tree-ring reconstructions of Colorado streamflow for water resource planning. Climate Change, 78, 293–315. doi: https://doi.org/10.1007/s10584-006-9055-0
Yocom, L. L., Fulé, P. Z., Brown, P. M., Cerano, J. N., Villanueva-Díaz, J., Falk, D. A., & Cornejo-Oviedo, E. (2010). El Niño–Southern Oscillation effect on a fire regime in northeastern Mexico has changed over time. Ecology, 91, 1660–1671. http://library.eri.nau.edu/gsdl/collect/erilibra/index/assoc/HASH0e72.dir/doc.pdf
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
Copyright (c) 2015 Revista Chapingo Serie Ciencias Forestales y del Ambiente