Climatic implications in earlywood and latewood width indices of Chinese pine in north central China

Kaixuan Yang1,2,3,4, Junzhou Zhang3,4(), Haowen Fan3,5, Yuan Yan3,4

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Journal of Forestry Research ›› 2024, Vol. 35 ›› Issue (1) : 50. DOI: 10.1007/s11676-024-01702-0

Climatic implications in earlywood and latewood width indices of Chinese pine in north central China

  • Kaixuan Yang1,2,3,4, Junzhou Zhang3,4(), Haowen Fan3,5, Yuan Yan3,4
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Abstract

Latewood width (LWW) indices of trees are considered a reliable proxy of summer precipitation in the Northern Hemisphere. However, the strong coupling and high correlation between earlywood width (EWW) and LWW indices often prevent registration of climate signals of the LWW index. In this study, 328-year-long earlywood width and latewood width chronologies were developed from Chinese pine at two sites in the Hasi Mountains, north central China. The climate responses of these chronologies were analyzed and the LWW index used to derive summer precipitation signals. Correlation analyses showed that LWW was particularly influenced by earlywood growth and recorded stronger climate signals of the previous year as EWW, rather than those of the current year with infrequent summer climate signals. However, after removing the effect of earlywood growth using a simple regression model, the adjusted LWW chronology (LWWadj) showed a strong relationship with July precipitation in dry years. This suggests that the LWWadj chronology has the potential to be used to investigate long-term variability in summer precipitation in drought-limited regions.

Keywords

Dendroclimatology / Latewood width / Climate response / Summer precipitation / Earlywood effect

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Kaixuan Yang, Junzhou Zhang, Haowen Fan, Yuan Yan. Climatic implications in earlywood and latewood width indices of Chinese pine in north central China. Journal of Forestry Research, 2024, 35(1): 50 https://doi.org/10.1007/s11676-024-01702-0

References

[1]
Albaugh TJ, Lee Allen H, Dougherty PM, Johnsen KH (2004) Long term growth responses of loblolly pine to optimal nutrient and water resource availability. For Ecol Manag 192:3–19. https://doi.org/10.1016/j.foreco.2004.01.002
[2]
Bing XJ, Yao QC, Zhou FF, Zheng ZP, Bai MW, Jiang SX, Wang CQ, Fang KY (2022) March–May snow cover extent reconstruction for the past four centuries based on the tree-ring early-wood on the southeastern Tibetan Plateau. Front Ecol Evol 10:900219. https://doi.org/10.3389/fevo.2022.900219
[3]
Bregy JC, Maxwell JT, Robeson SM, Harley GL, Elliott EA, Heeter KJ (2022) US Gulf Coast tropical cyclone precipitation influenced by volcanism and the North Atlantic subtropical high. Commun Earth Environ 3:164. https://doi.org/10.1038/s43247-022-00494-7
[4]
Chen FH, Yu ZC, Yang ML, Ito E, Wang SM, Madsen DB, Huang XZ, Zhao Y, Sato T, Birks HJB, Boomer I, Chen JH, An CB, Wuennemann B (2008) Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history. Quat Sci Rev 27:351–364. https://doi.org/10.1016/j.quascirev.2007.10.017
[5]
Chen F, Yuan YJ, Wei WS, Yu SL, Li Y, Zhang RB, Zhang TW, Shang HM (2010) Chronology development and climate response analysis of Schrenk spruce (Picea schrenkiana) tree-ring parameters in the Urumqi River basin, China. Geochronometria 36:17–22. https://doi.org/10.2478/v10003-010-0014-4
[6]
Chen F, Yuan YJ, Wen WS, Yu SL, Fan Z, Zhang RB, Zhang TW, Shang HM (2012) Tree-ring-based reconstruction of precipitation in the Changling Mountains, China, since A.D.1691. Int J Biometeorol 56:765–774. https://doi.org/10.1007/s00484-011-0431-8
[7]
Chen YP, Chen F, Zhang HL (2021) A tree-ring-based precipitation reconstruction since 1760 CE from northeastern Tibetan Plateau. China Atmosphere 12:416. https://doi.org/10.3390/atmos12040416
[8]
Cook ER (1985) A time series analysis approach to tree ring standardization. The University of Arizona
[9]
Crawford CJ, Griffin D, Kipfmueller KF (2015) Capturing season-specific precipitation signals in the northern Rocky Mountains, USA, using earlywood and latewood tree rings: Tree rings and seasonal precipitation. J Geophys Res Biogeosci 120:428–440. https://doi.org/10.1002/2014JG002740
[10]
Fritts HC (1966) Growth-rings of trees: their correlation with climate. Science 154:973–979. https://doi.org/10.1126/science.154.3752.973
[11]
Gou XH, Gao LL, Deng Y, Chen FH, Yang MX, Still C (2015) An 850-year tree-ring-based reconstruction of drought history in the western Qilian Mountains of northwestern China. Int J Climatol 35:3308–3319. https://doi.org/10.1002/joc.4208
[12]
Griffin D, Meko DM, Touchan R, Leavitt SW, Woodhouse CA (2011) Latewood chronology development for summer-moisture reconstruction in the US southwest. Tree-Ring Res 67:87–101. https://doi.org/10.3959/2011-4.1
[13]
Griffin D, Woodhouse CA, Meko DM, Stahle DW, Faulstich HL, Carrillo C, Touchan R, Castro CL, Leavitt SW (2013) North American monsoon precipitation reconstructed from tree-ring latewood. Geophys Res Lett 40:954–958. https://doi.org/10.1002/grl.50184
[14]
Guo BH, Nie JS, Stevens T, Buylaert JP, Peng TJ, Xiao WJ, Pan BT, Fang XM (2022) Dominant precessional forcing of the East Asian summer monsoon since 260 ka. Geology 50:1372–1376. https://doi.org/10.1130/G50206.1
[15]
Hoff C, Rambal S (2003) An examination of the interaction between climate, soil and leaf area index in a Quercus ilex ecosystem. Ann for Sci 60:153–161. https://doi.org/10.1051/forest:2003008
[16]
Holmes RL (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bull 43:51–67
[17]
Hughes MK, Wu XD, Shao XM, Garfin GM (1994) A preliminary reconstruction of rainfall in north-central China since A.D. 1600 from tree-ring density and width. Quat Res 42:88–99. https://doi.org/10.1006/qres.1994.1056
[18]
Kang SY, Yang B, Qin C (2012) Recent tree-growth reduction in north central China as a combined result of a weakened monsoon and atmospheric oscillations. Clim Change 115:519–536. https://doi.org/10.1007/s10584-012-0440-6
[19]
Koretsune S, Fukuda K, Chang ZY, Shi FC, Ishida A (2009) Effective rainfall seasons for interannual variation in δ 13 C and tree-ring width in early and late wood of Chinese pine and black locust on the Loess Plateau, China. J for Res 14:88–94. https://doi.org/10.1007/s10310-009-0111-2
[20]
Lin FY, Tan LC, Xue G, Cheng X, Zhang HW, Cheng H, Edwards RL, Wang TL, Li D, Gao YL, An ZS (2021) Seasonality of precipitation recorded in a modern (1907–2008) annually laminated stalagmite from central China. Palaeogeogr Palaeoclimatol Palaeoecol 576:110489. https://doi.org/10.1016/j.palaeo.2021.110489
[21]
Liu Y, Cai QF, Shi JF, Hughes MK, Kutzbach JE, Liu ZY, Ni FB, An ZS (2005) Seasonal precipitation in the south-central Helan Mountain region, China, reconstructed from tree-ring width for the past 224 years. Can J for Res 35:2403–2412. https://doi.org/10.1139/x05-168
[22]
Liu WH, Gou XH, Li JB, Huo YX, Yang MX, Zhang JZ, Zhang WG, Yin DC (2021) Temperature signals complicate tree-ring precipitation reconstructions on the northeastern Tibetan Plateau. Glob Planet Change 200:103460. https://doi.org/10.1016/j.gloplacha.2021.103460
[23]
Ma MM, Qu YP, Lyu J, Zhang XJ, Su ZC, Gao H, Yang XJ, Chen XX, Jiang TL, Zhang JX, Shen MY, Wang Z (2022) The 2022 extreme drought in the Yangtze River Basin: Characteristics, causes and response strategies. River 1:162–171. https://doi.org/10.1002/rvr2.23
[24]
Martin-StPaul N, Delzon S, Cochard H (2017) Plant resistance to drought depends on timely stomatal closure. Ecol Lett 20:1437–1447. https://doi.org/10.1111/ele.12851
[25]
Maxwell JT, Bregy JC, Robeson SM, Knapp PA, Soule PT, Trouet V, Affiliations AI (2021) Recent increases in tropical cyclone precipitation extremes over the US east coast. Proc Natl Acad Sci 118:e2105636118. https://doi.org/10.1073/pnas.2105636118
[26]
McDowell NG, Beerling DJ, Breshears DD, Fisher RA, Raffa KF, Stitt M (2011) The interdependence of mechanisms underlying climate-driven vegetation mortality. Trends Ecol Evol 26:523–532. https://doi.org/10.1016/j.tree.2011.06.003
[27]
Meko DM, Baisan CH (2001) Pilot study of latewood-width of conifers as an indicator of variability of summer rainfall in the North American monsoon region. Int J Climatol 21:697–708. https://doi.org/10.1002/joc.646
[28]
Miina J (2000) Dependence of tree-ring, earlywood and latewood indices of Scots pine and Norway spruce on climatic factors in eastern Finland. Ecol Model 132:259–273. https://doi.org/10.1016/S0304-3800(00)00296-9
[29]
Ming GD, Zhou WJ, Cheng P, Wang H, Xian F, Fu YC, Wu SG, Du H (2020) Lacustrine record from the eastern Tibetan Plateau associated with Asian summer monsoon changes over the past ~ 6 ka and its links with solar and ENSO activity. Clim Dyn 55:1075–1086. https://doi.org/10.1007/s00382-020-05312-4
[30]
Peng X, Yang B, Xiao S, Liu J, Li G (2021) Hydroclimate correlations between the alxa desert and adjacent mountains in Northwestern China: evidence from meteorological and tree ring data. J Geophys Res Atmosph 126:e2021JD05006. https://doi.org/10.1029/2021JD035006
[31]
Peng ZT, Zhang YD, Zhu LJ, Guo MM, Lu QG, Xu K, Shao H, Mo QF, Liu SR (2023) Spatial and temporal patterns of sensitivity of radial growth response by Picsea schrenkiana to regional climate change in the Tianshan Mountains. J Forestry Res 34:1669–1681. https://doi.org/10.1007/s11676-023-01629-y
[32]
Pompa-García M, Camarero JJ, Colangelo M, González-Cásares M (2021) Inter and intra-annual links between climate, tree growth and NDVI: improving the resolution of drought proxies in conifer forests. Int J Biometeorol 65:2111–2121. https://doi.org/10.1007/s00484-021-02170-5
[33]
Rico-Gray V, Palacios-Rios M (1996) Leaf area variation in Rhizophora mangle L. (Rhizophoraceae) along a latitudinal gradient in Mexico. Glob Ecol Biogeogr Lett 5:30. https://doi.org/10.2307/2997468
[34]
Sacher JA (1954) Structure and seasonal activity of the shoot apices of Pinus lambertiana and Pinus ponderosa. Am J Bot 41:749–759. https://doi.org/10.1002/j.1537-2197.1954.tb14406.x
[35]
Silkin PP, Kirdyanov AV (2003) The relationship between variability of cell wall mass of earlywood and latewood tracheids in larch tree-rings, the rate of tree-ring growth and climatic changes. Holzforschung 57:1–7. https://doi.org/10.1515/HF.2003.001
[36]
Song WQ, Zhao BQ, Mu CC, Ballikaya P, Cherubini P, Wang XC (2022) Moisture availability influences the formation and characteristics of earlywood of Pinus tabuliformis more than latewood in northern China. Agric for Meteorol 327:109219. https://doi.org/10.1016/j.agrformet.2022.109219
[37]
Stahle DW, Cleaveland MK, Grissino-Mayer HD, Griffin RD, Fye FK, Therrell MD, Burnette DJ, Meko DM, Villanueva Díaz J (2009) Cool- and warm-season precipitation reconstructions over Western New Mexico. J Clim 22:3729–3750. https://doi.org/10.1175/2008JCLI2752.1
[38]
Stokes MA, Smiley TL (1968) An Introduction to Tree-Ring Dating. Univ Ariz Press
[39]
Sucoff E (1971) Timing and rate of bud formation in Pinus resinosa. Can J Bot 49:1821–1832. https://doi.org/10.1139/b71-257
[40]
Torbenson MCA, Stahle DW, Villanueva Díaz J, Cook ER, Griffin RD (2016) The relationship between earlywood and latewood ring-growth across North America. Tree-Ring Res 72:53–66. https://doi.org/10.3959/1536-1098-72.02.53
[41]
Wang Y, Liu Y, Li Q, Song HM, Sun CF, Fang CX (2020) An asian summer monsoon-related relative humidity record from tree-ring δ18O in Gansu Province, north China. Atmosphere 11:984. https://doi.org/10.3390/atmos11090984
[42]
Wells N, Goddard S, Hayes MJ (2004) A self-calibrating palmer drought severity index. J Clim 17:2335–2351. https://doi.org/10.1175/1520-0442(2004)017%3c2335:ASPDSI%3e2.0.CO;2
[43]
Wigley TML, Briffa KR, Jones PD (1984) On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. J Appl Meteorol Climatol 23:201–213. https://doi.org/10.1175/1520-0450(1984)023%3c0201:OTAVOC%3e2.0.CO;2
[44]
Wu CY, Chen DS, Sun XM, Zhang SG (2023) Influence of altitude and tree class on climate-growth relationships in a larch plantation in subtropical China. J Forestry Res 34:1869–1880. https://doi.org/10.1007/s11676-023-01630-5
[45]
Xu JM, Bao FC, Lv JX, Huang RF, Zhao YK, Robert E (2013) Response to climate changes in radial growth of Picea crassifolia in the Qilian mountains of northwestern China. For Sci Pract 15:310–319. https://doi.org/10.1007/s11632-013-0418-0
[46]
Yang B, Kang SY, Ljungqvist FC, He MH, Zhao Y, Qin C (2014) Drought variability at the northern fringe of the Asian summer monsoon region over the past millennia. Clim Dyn 43:845–859. https://doi.org/10.1007/s00382-013-1962-y
[47]
Yang B, He MH, Yang L, Wang F, Ljungqvist FC (2023) Pine maximum latewood density in semi-arid Northern China records hydroclimate rather than temperature. Geophys Res Lett 50:e2023GL104362. https://doi.org/10.1029/2023GL104362
[48]
Yin DC, Gou XH, Yang HJ, Wang K, Liu J, Zhang YR, Gao LL (2023) Elevation-dependent tree growth response to recent warming and drought on eastern Tibetan Plateau. Clim Change 176:77. https://doi.org/10.1007/s10584-023-03542-z
[49]
Zaw Z, Fan ZX, Br?uning A, Liu WJ, Gaire NP, Than KZ, Panthi S (2021) Monsoon precipitation variations in Myanmar since AD 1770: linkage to tropical ocean-atmospheric circulations. Clim Dyn 56:3337–3352. https://doi.org/10.1007/s00382-021-05645-8
[50]
Zeng Q, Rossi S, Yang B (2018) Effects of age and size on xylem phenology in two conifers of Northwestern China. Front Plant Sci 8:2264. https://doi.org/10.3389/fpls.2017.02264
[51]
Zhang JZ, Gou XH, Alexander MR, Xia JQ, Wang F, Zhang F, Man ZH, Pedersom N (2021) Drought limits wood production of Juniperus przewalskii even as growing seasons lengthens in a cold and arid environment. CATENA 196:104936. https://doi.org/10.1016/j.catena.2020.104936
[52]
Zhao YS, Shi JF, Shi SY, Wang BW, Yu J (2017) Summer climate implications of tree-ring latewoossd width: a case study of Tsuga longibracteata in South China. Asian Geogr 34:131–146. https://doi.org/10.1080/10225706.2017.1377623
[53]
Zhao YS, Shi JF, Shi SY, Ma XQ, Zhang WJ, Wang BW, Sun XG, Lu HY, Br?uning A (2019) Early summer hydroclimatic signals are captured well by tree-ring earlywood width in the eastern Qinling Mountains, central China. Clim past 15:1113–1131. https://doi.org/10.5194/cp-15-1113-2019
[54]
Zhu LJ, Yao QC, Cooper DJ, Han SJ, Wang XC (2018) Response of Pinus sylvestris var. mongolica to water change and drought history reconstruction in the past 260 years, northeast China. Clim past 14:1213–1228. https://doi.org/10.5194/cp-14-1213-2018
[55]
Zhu LJ, Liu SG, Arzac A, Cooper DJ, Jin Y, Yuan DY, Zhu Y, Zhang X, Li ZS, Zhang YD, Liang HX, Wang XC (2021) Different response of earlywood vessel features of Fraxinus mandshurica to rapid warming in warm-dry and cold-wet areas. Agric for Meteorol 307:108523. https://doi.org/10.1016/j.agrformet.2021.108523
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