About this Journal Submit a Manuscript Table of Contents
International Journal of Forestry Research
Volume 2012 (2012), Article ID 467848, 7 pages
http://dx.doi.org/10.1155/2012/467848
Research Article

Influence of an Ice Storm on Aboveground Biomass of Subtropical Evergreen Broadleaf Forest in Lechang, Nanling Mountains of Southern China

1Graduate School of Human Sciences, Tokorozawa Campus, Waseda University, Mikajima 2-579-15, Tokorozawa 359-1192, Japan
2Division of Forest Ecosystem, Institute of Tropical Forest of China, No. 682, Longdong Guangshan No. 1 Road, Tianhe District, Guangzhou City, Guangdong Province 510-520, China
3Department of Environmental and Energy, Mitsubishi UFJ Research and Consulting Co. Ltd. 5-11-2, Toranomon, Minato-ku, Tokyo 105-8501, Japan

Received 22 April 2012; Revised 25 June 2012; Accepted 9 July 2012

Academic Editor: Guy R. Larocque

Copyright © 2012 Fang Zhang et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract

This study focuses on the influence of the 2008 ice storm in China and subsequent forest rehabilitation dynamics up until 2011. All seven plots studied exhibited significant damage, with the total number of damaged trees varying between 63 and 92%. In addition, most trees suffered stem bending in 2008 and the extent of damage varied with tree diameter at breast high (DBH). Relationships between loss of biomass as dead trees and stand characteristics were analyzed by multiple stepwise regression. The results showed that the decrease in biomass (Y) could be related to altitude (X1), slope (X2), and aboveground biomass (AGB) in 2008 (X5) according to the following formula: . After 2 to 3 years, tree numbers had declined in all seven plots. The mean increase in AGB (4.9 t ha−1) for six of the plots was less than the biomass loss as dead trees (9.4 t ha−1) over the 3 year periods. This corresponds to a release of CO2 to the atmosphere for each plot. Therefore, the forests of Lechang in the Nanling Montains have probably acted as a carbon source to the atmosphere for a short period after the 2008 ice storm.

1. Introduction

Almost 4,000 abiotic disturbance events occurred from 2000 to 2009, killing over one million people, directly affecting over 2.5 billion people and costing almost a trillion US dollars (over US$971 billion) [1]. Asia experienced the most extreme weather events during that period, with 1,536 events recorded, representing over 38% of the total worldwide. Windstorms and floods together accounted for approximately 70% of total extreme weather events reported and 72% of total economic loss. One such extreme weather event was the 2008 Chinese ice storm, which struck the southern-central region of China and occurred between January and February 2008. This meteorological disaster was characterized by frozen rain and snow with extreme low temperatures [2]. According to statistics released by the Ministry of Civil Affairs of China, the ensuing direct economic losses amounted to more than $22.3 billion and indirect losses may be even greater. In particular, twenty million hectares of forests were destroyed. At the time of the ice storm, most forests in the region were young or middle aged, which is perhaps the most productive stage of stand development. Unfortunately, the ice storm destroyed 30 years’ efforts to reforest the region and led to widespread crown decapitation, stem bending, trunk breakage, lodging, and uprooting. The damage to forests also caused secondary problems such as soil erosion and mudslides. Insect infestation and tree disease outbreaks resulted from the sudden increase in damaged or wounded trees. Forest fires increased in subsequent months because of the large accumulation of dead litter on the forest floor, which provided fuel for fires. For example, in the province of Hunan, the number of forest fires in March 2008 was eleven-times higher than the average for the previous 10 years and the fire area was five-times higher than the average [3].

It is possible that forests in southern China could act as carbon sources for many years after such severe large-scale damage as occurred in the 2008 ice storm. Before the storm, the forest in this region accounted for 65% of the total terrestrial carbon sink for the whole country [4]. The ability of forest ecosystems in this region to serve as a net carbon sink largely depends on forest rehabilitation or reestablishment. Therefore, accurate biomass estimation for tropical forests has received considerable attention in recent years to understand the impact of extreme weather events on ecosystems better [5]. Since extreme weather events are generally sudden, sporadic, and unpredictable, their impact is usually difficult to study. Considerable information may exist on individual events, but often little information is available on the impact of a specific event on forests. Global reporting of such effects, particularly quantitative information on the affected areas is usually infrequent and sporadic [6]. To date, very little research has been performed on the Chinese ice storm. For example, there have been only a few limited studies since 1980 into the damage of ice snow between 1982 and 1983 in the Daxinganling Mountains [7]. Although this area of research has attracted increased attention over recent years, studies concerning the effect on biomass are still extremely scarce. The present study investigated the impact of the 2008 ice storm and forest rehabilitation dynamics up until 2011 by evaluating the variation in aboveground biomass (AGB) of evergreen broadleaf forest. The aim of this work was to examine whether the AGB was recovering to levels prior to the ice storm or not. In addition, the impact of the 2008 ice storm was assessed based on tree numbers and AGB. Further, quantitative evaluation of the 2008 ice storm impact could provide a scientific basis for policy makers concerned with postdisaster vegetation recovery.

2. Materials and Methods

2.1. Study Site

Measurements were taken of seven plots located in subtropical secondary forest severely damaged during the ice storm in the Yangdongshan Shierdushui Forest Reserve (25°21′N, 113°25′E), Lechang, in the Nanling Mountains of southern China. The total area of this reserve is 11,651 hectares. It lies next to the border between the Guangdong and Hunan provinces. The climate and soil conditions are similar to the Yangdongshan Forest Reserve. The average annual temperature is around 19°C. The frost-free period lasts for 300 days. Annual precipitation is over 1,700 mm and the rainfall is generally concentrated between March and August. There are six vegetation types in the reserve: coniferous and broad-leaved mixed forest, coniferous forest, evergreen and deciduous forest, broad-leaved mixed forest, evergreen broad-leaved forest, shrubs, grass, and bamboo forest. The main vegetation type is subtropical evergreen broad-leaved forest. Since flora and fauna resources are abundant, the biodiversity is expected to be relatively high.

2.2. Plots

Seven rectangular plots (SD 01–07) each of 1200 m2 (40 × 30 m) were set out randomly in the Yangdongshan Shierdushui Forest Reserve and a total of 5178 trees were measured (Table 1). The seven plots had suffered different degrees of damage during the 2008 ice storm (see following section). A census of tree diameter at breast high (DBH) and tree species was conducted in every plot. Measurements of plots SD01-04 were obtained during April, 2008 and August, 2011, whereas, data for plots SD 05~07 were collected during July, 2009 and September, 2011.

tab1
Table 1: Specific information on the seven study plots in the Yangdongshan Shierdushui Forest Reserve in 2011.
2.3. Tree Numbers and Biomass Estimation

All surviving trees were classified according to the following six categories(1)Trunk breakage: trees with a break running across the main stem, which could be the result of construction damage. The damage was usually severe and possibly led to tree death. The damage was subdivided into two forms based on breakage position (Figures 1(a1) and 1(a2)). (2)Uprooting: trees tipped over and roots totally or partly exposed to the air (Figures 1(b1) and 1(b2)).(3)Lodging: trees fallen on the ground but roots not exposed to the air. Two situations occurred: small trees generally fell with their stems leaning on the ground (Figure 1(c1)), relatively large trees typically fell and leaned on other trees, but their stems were not bent and roots not exposed (Figure 1(c2)).(4)Stem bending: the drag force, bending moments, and stresses acting on tree stems caused relatively slight mechanical damage (Figure 1(d)). Damage mainly resulted from the pressure of snow cover as a direct factor. A further factor was indirectly caused by other fallen trees or broken branches. Generally, these trees were able to self-repair and regrow. The potential for restoration depended on tree species, bending degree, and so forth. (5)Crown breakage: trees with crowns damaged by mechanical forces. The damage was usually not serious and trees could potentially recover after the damage (Figure 1(e)).(6)Healthy: trees that were undamaged and survived the 2008 ice storm.

467848.fig.001
Figure 1: Five categories of damage.

After 2-3 years, the recovery status of trees was analyzed based on four factors: restoration of stem bending (Figure 2(f)), terminal shoot elongation (Figure 2(g)), sprouting shoot elongation (Figures 2(h1) and 2(h2)), and new trees. Newly dead or dying trees were also recorded in 2011 (Figure 2(i)).

467848.fig.002
Figure 2: Four types of recovery.

Biomass in four plots (SD01–04) in 2008 and 2011 was estimated using DBH census data for each year and the allometric equation AGB (kg) = 0.1378 (DBH (cm))2.3142 ( = 0.9776) [8]. No DBH census data was available in the other three plots (SD05–07) in 2008. Therefore, biomass in these plots in 2008 could not be calculated using the above equation. Instead, the average annual variation of biomass could be estimated from DBH census data for 2009 and 2011. Thus, the biomass in 2008 in SD05–07 was estimated by using biomass data for 2011 corrected for the variation of biomass over the three years. DBH data were collected by the Chinese Academy of Forestry in 2008 or 2009 and in the present study in 2011. The variation in biomass of each plot was analyzed based on the type of damage, recovery status, terrain, and other factors. In addition, relationships between the loss of biomass as dead trees and plot characteristics were analyzed by multiple stepwise regression analysis. Finally, the extent of forest rehabilitation was assessed as well as the variation in AGB.

3. Results and Discussion

3.1. Analysis of Damage Status

Firstly, all seven plots showed significant damage, with the total number of damaged trees varying between 63 and 92%. This indicates that subtropical evergreen forest in Yangdongshan Shierdushui Forest Reserve was severely affected by the 2008 ice storm. The majority of trees in each plot suffered stem bending in 2008 (Table 2). In addition, 89.8% of all trees were classified as having a DBH of ≤3 or 3.1–9.0 cm and damage status clearly varied with DBH class (Figure 3). Stem bending was the main form of damage for DBH classes of ≤3 and 3.1–9.0 cm. However, crown breakage was the main form of damage in the other three DBH classes of 9.1–15.0, 15.1–21.0, and ≥21.1 cm. Trunk breakage, uprooting, lodging, and healthy trees occurred for each DBH class, but their distribution varied slightly.

tab2
Table 2: Distribution of tree numbers according to the six categories of damage in the seven plots.
467848.fig.003
Figure 3: Distribution of trees and types of damage for different DBH classes.

Secondly, trees with crown breakage had the highest AGB in six of the studied plots, whereas in remaining plot SD06, the AGB of trees with crown breakage was almost the same as healthy trees, which displayed the highest AGB (Table 3). The reason for this is the highest AGB values primarily occurred for trees with ≥21.1 cm DBH in all the plots except for plot SD01 (Table 4). Trees in the ≥21.1 cm DBH class suffered from crown breakage more than any of the other five types of damage (Figure 3). Therefore, the variation in AGB over the next three years is likely to depend on the recovery status of those trees with crown breakage.

tab3
Table 3: Biomass distribution according to six categories of damage in the seven plots in 2008.
tab4
Table 4: Biomass distribution in different DBH classes for the seven plots in 2008.

Thirdly, there was generally a decreasing trend in damage from plot SD01 to plot SD07 (Table 2), although the reason for such a trend is difficult to explain with the data currently available. There was no clear explanation for this trend based on plot location or other plot characteristics (altitude, slope angle, etc.). As a direct consequence of the ice storm, biomass loss due to dead trees in 2011 varied among all seven plots (Table 6). Based on preliminary observations, there was no marked difference in species composition. The dominant species was Castanopsis fabric Hance, but a large proportion of the forest also comprised pioneer and late-succession tree species, such as Castanopsis fissa Rehder and E. H. Wilson, Manglietia chingii Dandy, and Alniphyllum fortunei Makino, in all seven plots. Therefore, the relationships between the biomass loss as dead trees and plot characteristics (AGB; slope; altitude; slope aspect; stand density) were analyzed using simple regression analysis in order to identify potential impact factors (Figure 4). The results showed that altitude, slope angle, and AGB in 2008 correlated strongly ( , 0.030, and 0.023, resp.), with the biomass of dead trees ( = 0.675, 0.643, and 0.697, resp.) In contrast, both the slope aspect and stand density appeared to have no link with the biomass of dead trees. Their corresponding (0.185 and 0.016) were far less than for the other three stand characteristics. In addition, their values (0.750 and 0.779) were considerably higher than 0.05.

467848.fig.004
Figure 4: Simple regression analysis of dead tree biomass (2011) at the stand level versus stand characteristics in 2008.

Regression models were generated to examine any relationship in further detail (Table 5). Based on the results of multiple stepwise regression, the best model was as follows: ( : altitude; : slope angle; : AGB in 2008). Even though increased, the significance was more than 0.05 when the slope aspect ( ) or stand density ( ) was included in the regression. Therefore, slope aspect ( ) and stand density ( ) could be disregarded.

tab5
Table 5: Multiple stepwise regression of dead tree biomass (2011) at the stand level versus five stand characteristics in 2008 (X1: altitude; X2: slope angle; X3: slope aspect; X4: stand density; X5: AGB in 2008).
tab6
Table 6: Variation in biomass and tree numbers following the 2008 ice storm.
3.2. Analysis of Recovery Status

Tree numbers declined up until 2011 in all seven plots following the 2008 ice storm. In addition, few new trees were observed after 2-3 years: the mean number was 149 ha−1, corresponding to only 2.9% of the total number of trees in the seven plots (Table 6). Trees dying during the three year period were largely responsible for the loss of AGB in the seven plots.

The AGB in four of the plots (SD01, 05, 06, and 07) in 2011 was greater than in 2008. Another two plots (SD02 and 03) had values similar to those in 2008. Therefore, following damage in the 2008 ice storm, the forest seems to have returned to the 2008 level with regard to AGB after 2-3 years. One exception was plot SD04, which had a lower AGB in 2011 than in 2008. The reason for this is not only a relatively lower survival rate for trees in plot SD04 (Table 6) but also a greater number of larger trees died than in other plots. In contrast, the recovery status of plots SD06 and 07 was clearly better than for the other plots due to relatively slight damage during the 2008 ice storm and a high survival rate of trees. In addition, the slope aspect of both the latter plots was south. Superior natural conditions, such as abundant sunshine on the slope, are likely to promote the growth of trees, biomass production, and accumulation.

The increase in AGB in plots SD01 and 06 (2.8 and 6.9 t ha−1, resp.) was less than the biomass loss of dead trees (9.8 and 8.9 t ha−1). Thus, these plots represent a net source of CO2 to the atmosphere. Further, AGB did not increase in plots SD02, 03, and 04 (−2.1, −1.7, and −16.7 t ha−1). In only two plots SD06 and 07 was the increase in AGB (12.4 and 17.7 t ha−1, resp.) greater than the biomass loss of dead trees (3.4 and 3.7 t ha−1). These results suggest that the secondary evergreen broadleaf forest in areas damaged by the 2008 ice storm may be acting as carbon sources rather than carbon sinks for a short period.

Based on the loss of tree numbers and AGB, some areas such as plot SD04 was not recovering well during three years. Regular monitoring on these areas is definitely needed in order to prevent forest degradation and secondary disasters (forest fire, plant diseases, insect damage, and so on). During the process of monitoring in the future, we could artificially plant some new trees if necessary. Various native tree species should be selected, so that the structure of plant community, which might be originally composed of shrubs and ferns, would be more complex and stable. Through this small scale of afforestation and/or reforestation, an appropriate biodiversity could weather against future natural disasters. In the same time, clearing forest litter would also be an effective measure for the control of forest disease and insects if there were a sign of plant disease or insect damage found in the forests [9, 10].

4. Conclusions

The main conclusions can be summarized as follows(1)Subtropical evergreen forest in Yangdongshan Shierdushui Forest Reserve was severely affected by the 2008 ice storm. Stem bending was the main form of tree damage. The proportions of other types of damage were relatively low and varied slightly among plots. In addition, there was a decreasing trend in damage from plot SD01 to plot SD07, although the reason for this trend is not yet clear. The loss of biomass as dead trees correlated with the initial AGB (in 2008), slope angle, and altitude, which could be represented by the formula ( : altitude; : slope angle; : AGB in 2008). (2)After 2-3 years, the subtropical evergreen broadleaf forest near Lechang, in the Nanling Mountainous region of southern China has basically returned to the 2008 level with regard to AGB. However, tree numbers were still decreasing in the seven plots. The forest has probably changed from a carbon sink to a carbon source because of the relatively large-scale tree death that has occurred during the three years postdisaster.(3)Since there were some areas such as plot SD04 which was not recovering well, regular monitoring on these areas is really necessary to prevent forest degradation and future forest disasters. Meanwhile, some specific corresponding measures such as afforestation and/or reforestation and clearing forest litter could be carried on during the process of monitoring in the future.

Acknowledgments

This research was carried out in cooperation with the Institute of Tropical Forest of China under Grants 2007DFA31070 from the International Cooperation Project of the Science and Technology Ministry, 2008KJCX012-02 from the Forestry Science and Technology Innovation Fund Project of Guangdong province, and RITFYWZX2011-12 from the noncommercial basic research fund project of Research Institute of the Tropical Forestry, Chinese Academy of Forestry.

References

  1. International Federation of Red Cross and Red Crescent Societies (IFRC & RCS), World Disasters Report-Focus on urban risk, Geneva, Switzerland, 2010.
  2. B. Zhou, L. Gu, Y. Ding et al., “The great 2008 Chinese ice storm its socioeconomic-ecological impact and sustainability lessons learned,” Bulletin of the American Meteorological Society, vol. 92, no. 1, pp. 47–60, 2011. View at Publisher · View at Google Scholar · View at Scopus
  3. M. Wang, L. Shu, Q. Wang et al., “Forest fire occurrence in short term under the impacts of snow damage in south China-Case study in Hunan Province,” Scientia Silvae Sinicae, vol. 44, pp. 64–68, 2008.
  4. S. Piao, J. Fang, P. Ciais et al., “The carbon balance of terrestrial ecosystems in China,” Nature, vol. 458, no. 7241, pp. 1009–1013, 2009. View at Publisher · View at Google Scholar · View at Scopus
  5. D. S. Lu, P. Mausel, E. Brondizio, and E. Moran, “Above-ground biomass estimation of succession and mature forests using TM images in the Amazon Basin,” in Proceedings of the International Symposium on Geospatial Theory, Processing and Applications, 2002.
  6. FAO, “Global Forest Resources Assessment 2010,” Main Report Forestry Paper no. 163, FAO, Rome, Italy, 2011.
  7. G. L. Pang, “The disaster of snow and ice in the region of Daxingan mountains,” Journal of Glaciology and Geocryology, vol. 9, pp. 53–54, 1987.
  8. F. Zhang, G. Y. Zhou, M. Hiratsuka, K. Tanaka, and Y. Morikawa, “Above-ground biomass of subtropical forests in Longwangtan, Guangdong, China,” In press.
  9. Y. D. Li, “The Nanling National Nature Reserve underwent the ice and snow disaster: the eco-sensitive area needed urgently to save,” Scientia Silvae Sinicae, vol. 44, no. 6, pp. 2–4, 2008.
  10. Y. Q. Luo, “Rethinking about the control of plant diseases and insect damage after the freezing rain and snow disaster in secondary forests,” Scientia Silvae Sincae, vol. 44, no. 4, pp. 6–7, 2008.