Abstract
Using unprecedented catalogues of past severe drought data for the Yucatan Peninsula between 1502 and 1900 coming from historical written documentation, we identified five conspicuous time lapses with no droughts between 1577–1647, 1662–1724, 1728–1764, 1774–1799 and 1855–1880, as well as time epochs with most frequent droughts between 1800 and 1850. Moreover, the most prominent periodicity of the historical drought time series was that of ∼40 years. Using the Palmer Drought Severity Index for the Yucatan Peninsula for the period 1921–1987 we found prominent negative phases between ∼1942–1946 and 1949–1952, 1923–1924, 1928–1929, 1935–1936, 1962–1963, 1971–1972 and 1986–1987. Two prominent periodicities clearly appear at ∼5 and 10 years. Most modern and historical severe droughts lasted 1 year, and share a quasi-decadal frequency. Also, in the first 66 years of the twentieth century the frequency of occurrence of severe drought has been lower compared with the nineteenth century. Some of the major effects and impacts of the most severe droughts in the Yucatan region are examined. We also studied the relation between historical and modern droughts and several large scale climate phenomena represented by the Atlantic Multidecadal Oscillation (AMO) and the Southern Oscillation Index (SOI). Our results indicate that historical droughts and the cold phase of the AMO coincide, while the influence of the SOI is less clear. The strongest coherence between historical droughts and AMO occurred at periodicities of ∼40 years. For modern droughts the coherence of a drought indicator (the Palmer Drought Severity Index) is similar with AMO and SOI, although it seems more sustained with the AMO. They are strongest at ∼10 years and very clearly with the AMO cold phase. Concerning the solar activity proxies and historical droughts, the coherence with a record of beryllium isotope Be10, which is a good proxy of cosmic rays, is higher than with Total Solar Irradiance. We notice that the strongest coherence between historical droughts and Be10 occurs at periods ∼60–64 years. When studying modern droughts and solar activity, frequencies of ∼8 years appear, and the coherences are similar for both sunspots and cosmic rays. Comparing natural terrestrial and solar phenomena, we found that the most sustained and strongest modulation of historical drought occurrence is at ∼60–64 years and is between the historical drought series and the solar proxy Be10. For modern droughts we notice that the coherence is similar among AMO, SOI and the solar indices. We can conclude that the sea surface temperatures (AMO) and solar activity leave their signal in terms of severe droughts in the Maya lands, however in the long term, the influence of the SOI on this type of phenomenon is less clear.
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References
Beer J (2000) Long-term indirect indices of solar variability. Space Sci Rev 94:53–66
Bracamonte P (1994) La memoria enclaustrada. Historia indígena de Yucatán, 1750–1915, Historia de los pueblos indígenas de México, CIESAS and INI, México, 253 pp
Cavazos T, Hastenrath S (1990) Convection and rainfall over Mexico and their modulation by the Southern Oscillation. Int J Climatol 10:377–386
Colle B, Moss C (1995) The structure and evolution of cold surges east of the Rocky Mountains. Mon Weather Rev 123:2577–2610
Daubechies I (1990) The wavelet transforms time–frequency localization and signal analysis. IEEE Trans Inf Theory 36:901–1004
Di Mego J, Basart L, Endersen W (1976) An examination of the frequency and mean conditions surrounding frontal incursions into the Gulf of Mexico and Caribbean Sea. Mon Weather Rev 104:709–718
Escobar A (2004) Desastres agrícolas en México. Catálogo histórico. Tomo II: Siglo XIX (1822–1900). Fondo de Cultura Económica and CIESAS, México, 280 pp
Farriss NM (1992) La sociedad maya bajo el dominio colonial. Alianza Editorial, Madrid, 653 pp
Florescano E (1980) Análisis históricos de las sequías en México. SARH Committee Plan Hidráulico Nacional, México
Folland CK, Palmer TN, Parker DE (1986) Sahel rainfall and worldwide sea temperatures. Nature 320:602–606
García-Acosta V, Pérez-Zevallos JM, Molina del Villar A (2003) Desastres agrícolas en México. Catálogo histórico. Tomo I: Épocas prehispánica y colonial (958–1822). Fondo de Cultura Económica and CIESAS, México, 506 pp
Gilman DL, Fuglister FH, Mitchell JM (1963) On the power spectrum of “red noise.” J Atmos Sci 20:182–-184
Goldenberg SB, Landsea CW, Mestas-Nuñez AM, Gray WM (2001) The recent increase in Atlantic hurricane activity: causes and implications. Science 293:474–479
Gray ST, Graumlich LJ, Betancourt JL, Pederson GT (2004) A tree-ring based reconstruction of the Atlantic Multidecadal Oscillation since 1567 A.D. Geophys Res Lett 31:L12205–L12208
Grinsted A, Moore J, Jevrejera S (2004) Application of the cross wavelet transform and wavelet coherence to geophysical time series. Nonlinear Process Geophys 11:561–566
Hasegawa H (2005) A wavelet analysis of transient spike trains of Hodgkin–Huxley neurons. http://arxiv.org/ps/cond-mat/0109444
Herrera G (2005) Caracterización Geográfica de la Sequía en México. Ph.D. thesis, Universidad Nacional Autónoma de México, Facultad de Filosofía y Letras, Colegio de Geografía
Hodell DA, Brenner M, Curtis JH (2004) Terminal classic drought in the northern Maya lowlands inferred from multiple sediment cores in lake Chichancanab (Mexico). Quat Sci Rev. doi: 10.1016/j.quascirev.2004.10.013
Holmes DG (2003) Pulse width modulation for power converters: principles and practice. Thomas A. Lipo, 724 pp
Huang J, Higuchi K, Shabbar A (1998) The relationship between the North Atlantic Oscillations and El Niño-Southern Oscillation. Geophys Res Lett 25:2707--2710
Hudgins L, Friebe C, Mayer M (1993) Wavelet transforms and atmospheric turbulence. Phys Rev Lett 71:3279--3282
Jáuregui E (1979) Some aspects of pluviometric fluctuations in Mexico during the last 100 years (in Spanish). Bol Inst Geogr (UNAM) 9:39–64
Jáuregui E (1995) Rainfall fluctuations and tropical storm activity in Mexico. Erdkunde 49:39–48
Jáuregui E (1997) Climate changes in Mexico during the historical and instrumental periods. Quat Int 7:43–44
Jones PD, Mann ME (2004) Climate over past millennia. Rev Geophys 42(2):RG2002, doi: 10.1029/2003RG000143
Jones PD, Osborn TJ, Briffa KR (2003) Pressure-based measures of the North Atlantic Oscillation (NAO): a comparison and an assessment of changes in the strength of the NAO and in its influence on surface climate parameters. In: Hurrell JW, Kushnir Y, Ottersen G, Visbeck M (eds) The North Atlantic Oscillation, climate significance and environmental impact. Geophys Monogr 134:51–62
Kerr RA (2000) A North Atlantic climate pacemaker for centuries. Science 288:1984–1986
Klaus D (1973) Cold polar outbreaks in the tropics forming on the leeward of the Rocky Mountains. Geofís Int 13:99–143 (in Spanish)
Labat D, Ababou R, Mangin A (2000) Rainfall-runoff relations for karstic springs. Part II: continuous wavelet and discrete orthogonal multiresolution. J Hydrol 238:149--178
Lean J (2000) Evolution of the Sun’s spectral irradiance since the Maunder minimum. Geophys Res Lett 27:2425–2428
Lau K-M, Weng H-Y (1995) Climate signal detection using wavelet transform: how to make a time series sing. Bull Am Meteorol Soc 76:2391–2402
Magaña V, Amador J, Medina S (1999) The midsummer droughts over Mexico and Central America. J Climate 12:1577–1588
Magaña V, Vázquez J, Pérez J, Pérez JB (2003) Impact of el Niño on precipitation in Mexico. Geofis Int 42:313–330
McCabe G, Palecki M, Betancourt JL (2004) Pacific and Atlantic Ocean influences on multi-decadal drought frequency in the United States. Proc Natl Acad Sci U S A 101:4136–4141
Mendoza B, Jáuregui E, Díaz-Sandoval R, García-Acosta V, Velasco V, Cordero G (2005) Historical droughts in central Mexico and their relation with El Niño. J Appl Meteorol 44:709–716
Mendoza B, Velasco V, Jáuregui E (2006) A study of historical droughts in southeastern Mexico. J Climate 19:2916–2934
Mosiño P, García E (1966) The midsummer droughts in Mexico. In: Proc. Regional Latinamerican Conference, Int. Geophys. Union, Latin American Chapter 3, pp 500–516
Ogurtsov MG, Nagovitsyn YuA, Kocharov GE, Jungner H (2002) Long-period cycles of the sun’s activity recorded in direct solar data and proxies. Sol Phys 211:371–394
Ortlieb L (2000) The documented historical record of El Niño events in Peru: An update of the Quinn record (sixteenth through nineteenth centuries). In: Diaz HF, Markgraf V (eds) El Niño and the Southern Oscillation Multiscale Variability and Global and Regional Impact. Cambridge University Press, pp 207–295
Pozo-Vazquez D, Esteban-Parra M, Rodrigo F, Castro-Diez Y (2001) A study of NAO variability and its possible non-linear influences on European surface temperature. Clim Dyn 17:701--715
Quinn WH, Neal VT (1992) The historical record of El Niño events. In: Bradley RS, Jones PD (eds) Climate since a.d. 1500. Routledge, London, pp 623–648
Ropelewski C, Halpert M (1986) North American precipitation and temperature patterns associated with El Niño/Southern Oscillation (ENSO). Mon Weather Rev 114:2353–2362
Ropelewski C, Halpert M (1989) Precipitation patterns associated with the high phase of the Southern Oscillation. J Climate 2:268–284
Schlesinger ME, Ramankutty N (1994) An oscillation in the global climate system of periods 65–70 years. Nature 367:723–726
Schultz D, Bracken E, Bosart L, Hakim G, Bedrick M, Dickinson M, Tyle K (1997) The 1993 superstorm cold surge frontal structure and tropical impact. Mon Weather Rev 125:5–39
Torrence C, Compo G (1998) A practical guide to wavelet analysis. Bull Am Meteorol Soc 79:61–78
Torrence C, Webster P (1999) Interdecadal changes in the ENSO–monsoon system. J Clim 12:2679–2690
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Mendoza, B., García-Acosta, V., Velasco, V. et al. Frequency and duration of historical droughts from the 16th to the 19th centuries in the Mexican Maya lands, Yucatan Peninsula. Climatic Change 83, 151–168 (2007). https://doi.org/10.1007/s10584-006-9232-1
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DOI: https://doi.org/10.1007/s10584-006-9232-1