Advances in flash flood research based on dendrogeomorpholog

Jiazhi Qie, Yong Qie

Article ID: 1310
Vol 4, Issue 2, 2021, Article identifier:50-61

VIEWS - 67 (Abstract) 11 (PDF)


Flash flood is one of the major natural hazards in China. It seriously threatens the lives of people and property in mountainous areas. Various methods have been developed for flash flood study, but most of them focused on the past few decades. As one of the effective methods of historical flash flood events reconstruction, dendrogeomorphology has been used worldwide. It can provide hazard information with long temporal scale and high temporal resolution, sometimes at the seasonal level. By comparing tree ring width and other growth characteristics between disturbed and undisturbed trees, growth disturbance signals can be found in the disturbed trees. Using the growth disturbance in tree rings, flash flood events can be dated, and then the frequency, size, and spatial distribution characteristics of flash floods that have no or little documentary records can be reconstructed. The discharge of flash flood can be reconstructed quantitatively according to the height of scars or by using hydraulic models. With the development of dendrogeomorphology, research tends to probe into the meteorological driving mechanism of flash floods and the pattern of flash floods on a larger spatial scale. In the practical application of dendrogeomorphology, more instrumental data and historical records are applied in the studies. This makes the method increasingly more widely used around the world. But work based on dendrogeomorphology has not been reported in China. In this article, we reviewed the development of the study on flash floods based on tree ring, briefly summarized the research progress, and discussed the advantages, limitations, and potential of this approach, so as to provide some reference information for relevant work in China.


Flash Floods; Tree Ring; Dendrogemorpholog

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Collier CG. Flash flood forecasting: What are the limits of predictability? Quarterly Journal of the Royal Meteorological Society 2007; 133: 3–23.

Georgakokoskp. On the design of a national real-time early warning system with site-specific lightning flood forecasting capability. Bulletin of the American Meteorological Society 1986; 67(10): 1233–1239.

Zhao S. Preliminary study on the overall characteristics and risk zoning of flash flood disaster system in China. Journal of Natural Disasters 1996; 5(3): 93–99.

Gao Y, Xing J, Wang C, et al. Cause and forecast of flash flood from rainstorm. Journal of Natural Disasters 2006; 15(4): 65–70.

Zhou C, Jin S. Damage cause and control measures of flash flood hazard in Henan Province. Journal of Natural Disasters 2008; 17(3): 148–151.

Liu C, Miao T, Chen H, et al. Basic feature and origin of the”8·8” flash flood- debris flow disaster happened in Zhouqu County, Gansu, China, Aug. 8, 2010. Geological Bulletin of China 2011; 30(1): 141–150.

Zhang P, Ren H, Hu W, et al. An elementary study on Chinese flash floods disaster prevention regionalization. Journal of Soil and Water Conservation 2006; 20(6): 196–200.

Li Z, Yang D W, Hong Y, et al. Characterizing spatiotemporal variations of hourly rainfall by gauge and radar in the mountainous three gorges region. Journal of Applied Meteorology and Climatology 2014; 53(4): 873–889.

Liu Y S, Yuan X M, Guo L, et al. Driving force analysis of the temporal and spatial distribution of flash floods in Sichuan Province. Sustainability 2017; 9: 1527. doi: 10.3390/su9091527.

Jiang J, Shao L. Standard of flash flood warning based on the precipitation observation data. Journal of Hydraulic Engineering 2010; 41(4): 458–463.

Cheng W. A review of rainfall thresholds for triggering flash floods. Advances in Water Science 2013; 24(6): 901–908.

Li Q, Wang Y, Li H, et al. Rainfall threshold for flash flood early warning based on flood peak modulus. Journal of Geo-information Science 2017; 19(12): 1643–1652.

Tang C, Shi Y. Approach to mutil-objectives assessment for urban torrent hazard. Progress in Geography 2006; 25(4): 13–21.

Tang C, Zhu J. A GIS based regional torrent risk zonation. Acta Geographica Sinica 2005; 60(1): 87–94.

Chen H, Yang D W, Hong Y, et al. Hydrological data assimilation with the ensemble square-root-filter: Use of streamflow observations to update model states for real-time flash flood forecasting. Advances in Water Resources 2013; 59: 209–220.

Huang W, Cao Z, Qi W J, et al. Full 2D hydrodynamic modelling of rainfall-induced flash floods. Journal of Mountain Science 2015; 12(5): 1203–1218.

Cui P, Zou Q. Theory and method of risk assessment and risk management of debris flows and flash floods. Progress in Geography 2016; 35(2): 137–147.

George S, Nielsen E. Palaeoflood records for the Red River, Manitoba, Canada, derived from anatomical tree ring signatures. The Holocene 2003; 13(4): 547–555.

Ballesteros-Cánovas JA, Rodríguez-Morata C, GarófanoGómez V, et al. Unravelling past flash flood activity in a forested mountain catchment of the Spanish Central System. Journal of Hydrology 2014; 529: 468–479.

Stoffel M. Dating past geomorphic processes with tan-gential rows of traumatic resin ducts. Dendrochronologia 2008; 26(1): 53–60.

Wang Z, Qian Y. Frequency and intensity of extreme precipitation events in China. Advances in Water Science 2009; 20(1): 1–9.

She D, Xia J, Zhang Y, et al. The trend analysis and statistical distribution of extreme rainfall events in the Huaihe River Basin in the past 50 years. Acta Geographica Sinica 2011; 66(9): 1200–1210.

Ren Z, Zhang M, Wang S, et al. Changes in precipitation extremes in South China during 1961–2011. Acta Geographica Sinica 2014; 69(5): 640–649.

Fritts HC. Tree rings and climate. London, UK: Academic Press; 1976.

Alestalo J. Dendrochronological interpretation of geomorphic processes. Fennia 1971; 105: 1–139.

Butler DR. Snow avalanche path terrain and vegetation, Glacier National Park, Montana. Arctic and Alpine Research 1979; 11(1): 17–32.

Hupp CR. Dendrogeomorphic evidence of debris flow frequency and magnitude at Mount Shasta, California. Environmental Geology and Water Sciences 1984; 6(2): 121–128.

Stoffel M. A review of studies dealing with tree rings and rockfall activity: The role of dendrogeomorphology in natural hazard research. Natural Hazards 2006; 39(1): 51–70.

Hardman G. The relationship between tree growth and stream runoff in the Truckee River Basin, California-Nevada. Transactions, American Geophysical Union 1936; 17(2): 491–493.

Sigafoos RS. Vegetation in relation to flood frequency near. Washington DC, USA: United States Government Printing Office; 1961.

Sigafoos RS. Botanical evidence of floods and floodplain deposition. Washington DC, USA: United States Government Printing Office; 1964.

Baker VR. Palaeoflood hydrology and extraordinary flood events. Journal of Hydrology 1987; 96: 79–99.

Bégin Y. Tree-ring dating of extreme lake levels at the subarcticboreal interface. Quaternary Research 2001; 55(2): 133–139.

Zielonka T, Holeksa J, Ciapala S. A reconstruction of flood events using scarred trees in the Tatra Mountains, Poland. Dendrochronologia 2008; 26(3): 173–183.

Ruiz-Villanueva V, Díez-Herrero A, Stoffel M, et al. Dendrogeomorphic analysis of flash floods in a small ungauged mountain catchment (Central Spain). Geomorphology 2010; 118(3-4): 383–392.

Ballesteros JA, Stoffel M, Bodoque JM, et al. Changes in wood anatomy in tree rings of Pinus pinaster Ait following wounding by flash floods. Tree-Ring Research 2010; 66(2): 93–103.

Ballesteros JA, Stoffel M, Bollschweiler M, et al. Flash flood impacts cause changes in wood anatomy of Alnus glutinosa, Fraxinus angustifolia and Quercus pyrenaica. Tree Physiology 2010; 30(6): 773–781.

Ferrio JP, Díez-Herrero A, Tarrés D, et al. Using stable isotopes of oxygen from tree-rings to study the origin of past flood events: First results from the Iberian Peninsula. Quaternaire 2015; 26(1): 67–80.

Ballesteros-Cánovas JA, Eguibar M, Bodoque JM, et al. Estimating flash flood discharge in an ungauged mountain catchment with 2D hydraulic models and dendrogeomorphic palaeostage indicators. Hydrological Processes 2011; 25(6): 970–979.

Ballesteros-Cánovas JA, Stoffel M, Guardiola-Albert C.XRCT images and variograms reveal 3D changes in wood density of riparian trees affected by floods. Trees 2015; 29(4): 1115–1126.

Grissino-Mayer HD. A manual and tutorial for the proper use of an increment borer. Tree-Ring Research 2003; 59(2): 63–79.

Schneuwly DM, Stoffel M, Dorren LK, et al. Three-dimensional analysis of the anatomical growth response of European conifers to mechanical disturbance. Tree Physiology 2009; 29(10): 1247–1257.

Schneuwly DM, Stoffel M, Bollschweiler M. Formation and spread of callus tissue and tangential rows of resin ducts in Larix decidua and Picea abies following rockfall impacts. Tree Physiology 2009; 29(2): 281–289.

Grissino-Mayer HD. Evaluating crossdating accuracy: Amanual and tutorial for the computer program cofecha. Tree-Ring Research 2001; 57: 205–221.

Gottesfeld AS. British Columbia flood scars: Maximum flood-stage indicator. Geomorphology 1996; 14: 319–325.

George SS. Tree rings as paleoflood and paleostage indicators. Tree Rings and Natural Hazards 2010; 41: 233–239.

Stoffel M, Wilford DJ. Hydrogeomorphic processes and vegetation: Disturbance, process histories, dependencies and interactions. Earth Surface Processes and Landforms 2012; 37: 9–22.

Stoffel M, Casteller A, Luckman B H, et al. Spatiotemporal analysis of channel wall erosion in ephemeral torrents using tree roots: An example from the Patagonian Andes. Geology 2012; 40(3): 247–250.

Stoffel M, Butler DR, Corona C. Mass movements and tree rings: A guide to dendrogeomorphic field sampling and dating. Geomorphology 2013; 200: 106–120.

Yamamoto F, Kozlowski TT. Effects of flooding, tilting of stems, and ethrel application on growth, stem anatomy and ethylene production of pinus densiflora seedlings. Journal of Experimental Botany 1987; 38: 293–310.

Friedman JM, Vincent KR, Shafroth PB. Dating floodplain sediments using tree-ring response to burial. Earth Surface Processes and Landforms 2005; 30(9): 1077–1091.

Kogelnig-Mayer B, Stoffel M, Schneuwly-Bollschweiler M, et al. Possibilities and limitations of dendrogeomorphic time-series reconstructions on sites influenced by debris flows and frequent snow avalanche activity. Arctic, Antarctic, and Alpine Research 2011; 43(4): 649–658.

Stoffel M, Corona C. Dendroecological dating of geomorphic disturbance in trees. Tree-Ring Research 2014; 70(1): 3–20.

Schneuwly-Bollschweiler M, Corona C, Stoffel M. Howto improve dating quality and reduce noise in tree-ring based debris-flow reconstructions. Quaternary Geochronology 2013; 18: 110–118.

Casteller A, Stoffel M, Crespo S, et al. Dendrogeomorphic reconstruction of flash floods in the Patagonian Andes. Geomorphology 2015; 228: 116–123.

Shroder JF. Dendro-geomorphological analysis of mass movement on Table Cliffs Plateau, Utah. Quaternary Research 1978; 9(2): 168–185.

Butler DR, Malanson GP. A reconstruction of snow-avalanche characteristics in Montana, USA using vegetative indicators. Journal of Glaciology 1985; 31: 185–187.

Šilhán K. Frequency, predisposition, and triggers of floods in flysch Carpathians: Regional study using dendrogeomorphic methods. Geomorphology 2015; 234: 243–253.

Ruiz-Villanueva V, Diez-Herrero A, Bodoque J M, et al. Characterisation of flash floods in small ungauged mountain basins of Central Spain using an integrated approach. Catena 2013; 110: 32–43.

Ballesteros-Cánovas JA, Czajka B, Janecka K, et al. Flash floods in the Tatra Mountain streams: Frequency and triggers. Science of the Total Environment 2015; 511: 639–648.

Rodriguez-Morata C, Ballesteros-Cánovas JA, Trappmann D, et al. Regional reconstruction of flash flood history in the Guadarrama range (Central System, Spain). Science of the Total Environment 2016; 550: 406–417.

Harrison SS, Reid JR. A flood-frequency graph basedon tree-scar data. Proceedings of the Northern Dakota Academy of Sciences 1967; 21: 23–33.

McCord VA. Fluvial process dendrogeomorphology: Reconstructions of flood events from the southwestern United States using flood-scarred trees. Dean JS, MekoDM, Swetnam TW. Tree rings, environment and humanity. Tucson, USA: University of Arizona; 1996. p. 689–699.

Jarrett RD, England J. Reliability of paleostage indicators for pale of lood studies. House PK, Webb RH, Baker VR, et al. Ancient floods, modern hazards: Principles and applications of paleoflood hydrology. Water science and application Vol. 5.Washington DC, USA: American Geophysical Union; 2002. p. 91–109.

Ballesteros-Cánovas JA, Trappmann D, Shekhar M, et al. Regional flood-frequency reconstruction for Kullu district, Western Indian Himalayas. Journal of Hydrology 2017; 546: 140–149.

Webb RH, Jarrett RD. One-dimensional estimation techniques for discharges of paleofloods and historical floods. House PK, Webb RH, Baker VR, et al. Ancient floods, modern hazards: Principles and applications of paleoflood hydrology. Water Science and Application, vol. 5. Washington D C, USA: American Geophysical Union; 2002. p. 111–125.

Darby S. Effect of riparian vegetation on flow resistence and flood potential. Journal of Hydraulic Engineering 1999; 125(5): 443–454.

Carling PA, Hoffman M, Blatter AS. Initial motion of boulders in bedrock channel. House PK, Webb RH, Baker VR, et al. (editors). Ancient floods, modern hazards: Principles and applications of pale of lood hydrology. Water Science and Application, vol. 5. Washington D C, USA: American Geophysical Union; 2002. p. 147–160.

Ballesteros JA, Bodoque JM, Díez-Herrero A, et al. Calibration of floodplain roughness and estimation of flood discharge based on tree-ring evidence and hydraulic modelling. Journal of Hydrology 2011; 403(1-2): 103–115.

Ballesteros-Cánovas JA, Márquez-Peñaranda JF, SánchezSilva M, et al. Can tree tilting be used for pale of flood discharge estimations? Journal of Hydrology 2015; 529: 480–489.

Guo L, Zhang X, Liu R, et al. Achievements and preliminary analysis on China national flash flood disasters investigation and evaluation. Journal of Geo- information Science 2017; 19(12): 1548–1556.

Shao XM, Xu Y, Yin ZY, et al. Climatic implications ofa 3585-year tree-ring width chronology from the northeastern Qinghai-Tibetan Plateau. Quaternary Science Reviews 2010; 29: 2111–2122.

Yang B, Qin C, Wang JL, et al. A 3,500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau. PNAS 2014; 111(8); 2903–2908.

Zhang QB, Evans MN, Lyu LX. Moisture dipole over the Tibetan Plateau during the past five and a half centuries. Nature Communications 2015; 6: 8062. doi: 10.1038/ncomms9062.

Liang EY, Wang YF, Piao SL. Species interactions slow warming-induced upward shifts of treelines on the Tibetan Plateau. PNAS 2016; 113(16): 4380–4385.

Liu Y, Cobb KM, Song HM, et al. Recent enhancement of central Pacific EI Niño variability relative to last eight centuries. Nature Communications 2017; 8: 15386. doi: 10. 1038/ncomms15386.

Han T. The dendrochronological method: A new method for determining the ages of seismic deformational belts in Damxung of Xizang (Tibet). Journal of the Chinese Academy of Geological Sciences 1983; (6): 95–110.

Han T. Discussion on epicentral locations for the Tibet M=8 earthquake on 29, September 1411. Seismology and Geology 1984; 6(4): 6–12.

Yang B, Liu B, Zhou J. Tree seismological study of active Gulang and Jingtai fault in Gansu Province. Seismology and Geology 1995; 17(2): 139–147.

Lin AM, Lin SJ. Tree damage and surface displacement: The 1931 M 8.0 Fuyun earthquake. The Journal of Geology 1998; 106: 751–757.

Hong T, Bai S, Wang J, et al. Reconstruct the activity years of Jiufangshan landslide by means of tree- rings. Journal of Mountain Science 2012; 30(1): 57–64.

Tie Y, Malik I, Owczarek P. Dendrochronological dating of debris flow historical events in high mountain area: Take Daozao debris flow as an example. Mountain Research 2014; 32(2): 226–232.

Malik I, Wistuba M, Tie YB, et al. Mass movements of differing magnitude and frequency in a developing highmountain area of the Moxi Basin, Hengduan Mts, China: A hazard assessment. Applied Geography 2017; 87: 54–65.

Yang B, Bräuning A, Dong ZB, et al. Late Holocene monsoonal temperate glacier fluctuations on the Tibetan Plateau. Global and Planetary Change 2008; 60: 126–140.

Xu P, Zhu H, Shao X, et al. Tree ring-dated fluctuation history of Midui glacier since the Little Ice Age in the southeastern Tibetan Plateau. Science China: Earth Sciences 2012; 42(3): 380–389.

Zhu HF, Shao XM, Zhang H, et al. Trees record changes of the temperate glaciers on the Tibetan Plateau: Potential and uncertainty. Global and Planetary Change 2019; 173: 15–23.

Zhu HF, Xu P, Shao XM, et al. Little Ice Age glacier fluctuations reconstructed for the southeastern Tibetan Plateau using tree rings. Quaternary International 2013; 283: 134–138.

Zhang Y, Stoffel M, Liang E Y, et al. Centennial-scale process activity in a complex landslide body in the Qilian Mountains, northeast Tibetan Plateau, China. Catena 2019; 179: 29–38.



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