热带喀斯特森林多花白头树木质部年内生长动态及其对环境因子的响应

多花白头树(Garuga floribunda var.gamblei)是西双版纳热带喀斯特森林中常见的落叶树种,容易受水分亏缺的影响。为探究热带喀斯特森林树木年内生长动态及其对环境因子的响应,该研究利用生长环和微树芯两种方法监测了多花白头树在2020—2021年的树干径向变化和木质部生长动态,并分析了树干径向变化和木质部生长与环境因子的相关性。微树芯法的监测表明,在2020年,多花白头树在3月底开始出现扩大细胞,9月底细胞壁加厚结束;在2021年,多花白头树在4月中旬开始出现扩大细胞,10月中旬细胞壁加厚结束。生长环的监测表明,2020年和2021年的径向生长开始时间均晚于扩大细胞出现时间,径向生长结束时间均早于细胞壁加厚结束时间。多花白头树在2020年和2021年的木质部生长持续时间大致相同,2020年的木质部生长量((2.87±1.46)mm)也与2021年((2.98±1.02)mm)几乎一致。多花白头树的月径向生长量、扩大细胞区域宽度和细胞壁加厚区域宽度均与降水呈显著正相关,这表明水分状况在多花白头树的木质部生长过程中发挥了重要作用;扩大细胞区域宽度还与日平均气温和日最低温显...     

热带季节雨林多花白头树年内径向生长动态及其对环境因子的响应

为了解热带地区树木的季节性生长动态和规律,在西双版纳热带季节雨林利用高精度生长仪和微树芯法对落叶树种多花白头树的径向生长季节动态进行监测。结合木质部非结构性碳水化合物和环境因子的监测,分析其形成层活动和径向季节动态的生理生态驱动因子。结果表明: 在2020年,生长仪的监测显示,多花白头树于5月底(儒略日DOY:149.3±7.2)开始生长,8月底(DOY:241.0±14.7)生长结束,年生长量为3.12 mm,最大生长速率为0.04 mm·d^-1。而微树芯法显示,扩大细胞3月9日(DOY:69.2±6.2)开始出现,9月19日(DOY:262.8±2.8)细胞加厚结束,木质部生长量为1.76 mm,最大生长速率为0.009 mm·d^-1。多花白头树径向日生长量与生长季的降水、相对湿度、日最低气温、深度为20 cm的土壤含水量和温度呈显著正相关,而与日最高气温、水汽压亏缺、最大风速和水汽压呈显著负相关。多花白头树边材淀粉含量和可溶性糖含量均在生长季开始之前保持较高水平,淀粉含量在3月底达到最低,而可溶性糖含量5月中旬达到最低,随着生长季的结束淀粉和可溶性糖的含量分别在10月中旬和12月底达到最高。     

How needle phenology indicates the changes of xylem cell formation during drought stress in Pinus sylvestris L.

Temperature, water availability and photoperiod are the primary drivers of tree phenological processes. However, there is lack of information how the spring temperature and summer drought affect phenology of both cambium and needles. We evaluated the interplay between xylem and needle development of mature Scots pine trees in three consecutive years differing in the spring temperatures and onset and duration of summer drought. Cambial activity began on the day of a year (DOY) 83–87, while the bud break occurred on DOY 113–119, when also the secondary cell wall of tracheids started its formation. While the timing of bud break correlated with the sum of effective temperatures, the beginning of cambial zone activity did not. The needles were fully unfolded around DOY 170, which corresponded to the transition between earlywood and latewood tracheids. Summer drought did not affect needle development, but it changed the rate of production and morphology of latewood tracheids. Latewood tracheids from the year 2015 when the drought was longest (i.e. until the second half of August in 2015 compared to the duration from June until the middle of July in the two other years) were 32% narrower and they had 34% thinner cell walls than in 2014 and 2016. The improvement of tree water status in July resulted in the formation of intra-annual density fluctuations (IADF). The interplay between needle and cambium phenology provided an insight into how the tree allocates the resources with varying temperature and soil water availability.     

Temporal dynamic of wood formation in Pinus cembra along the alpine treeline ecotone and the effect of climate variables

We determined the temporal dynamic of cambial activity and xylem development of stone pine (Pinus cembra L.) throughout the treeline ecotone. Repeated micro-sampling of the developing tree ring was carried out during the growing seasons 2006 and 2007 at the timberline (1,950 m a.s.l.), treeline (2,110 m a.s.l.) and within the krummholz belt (2,180 m a.s.l.) and the influence of climate variables on intra-annual wood formation was determined. At the beginning of both growing seasons, highest numbers of cambial and enlarging cells were observed at the treeline. Soil temperatures at time of initiation of cambial activity were c. 1.5°C higher at treeline (open canopy) compared to timberline (closed canopy), suggesting that a threshold root-zone temperature is involved in triggering onset of above ground stem growth. The rate of xylem cell production determined in two weekly intervals during June through August 2006–2007 was significantly correlated with air temperature (temperature sums expressed as degree-days and mean daily maximum temperature) at the timberline only. Lack of significant relationships between tracheid production and temperature variables at the treeline and within the krummholz belt support past dendroclimatological studies that more extreme environmental conditions (e.g., wind exposure, frost desiccation, late frost) increasingly control tree growth above timberline. Results of this study revealed that spatial and temporal (i.e., year-to-year) variability in timing and dynamic of wood formation of P. cembra is strongly influenced by local site factors within the treeline ecotone and the dynamics of seasonal temperature variation, respectively.     

Evidence of threshold temperatures for xylogenesis in conifers at high altitudes

Temperature is the most important factor affecting growth at high altitudes. As trees use much of the allocated carbon gained from photosynthesis to produce branches and stems, information on the timing and dynamics of secondary wood growth is crucial to assessing temperature thresholds for xylogenesis. We have carried out histological analyses to determine cambial activity and xylem cell differentiation in conifers growing at the treeline on the eastern Alps in two sites during 2002–2004 with the aim of linking the growth process with temperature and, consequently, of defining thresholds for xylogenesis. Cambial activity occurred from May to July–August and cell differentiation from May–June to September–October. The earliest start of radial enlargement was observed in stone pine in mid-May, while Norway spruce was the last species to begin tracheid differentiation. The duration of wood formation varied from 90 to 137 days, depending on year and site, with no difference between species. Longer durations were observed in trees on the south-facing site because of the earlier onset and later ending of cell production and differentiation. The threshold temperatures at which xylogenesis had a 0.5 probability of being active were calculated by logistic regressions. Xylogenesis was active when the mean daily air temperature was 5.6–8.5°C and mean stem temperature was 7.2–9°C. The similar thresholds among all trees suggested the existence of thermal limits in wood formation that correspond with temperatures of 6–8°C that are supposed to limit growth at the treeline. Different soil temperature thresholds between sites indicated that soil temperature may not be the main factor limiting xylogenesis. This study represents the first attempt to define a threshold through comparative assessment of xylem growth and tissue temperatures in stem meristems at high altitudes.     

长白山北坡不同年龄红松年表及其对气候的响应

运用树木年轮气候学方法,研究了长白山北坡红松(Pinus koraiensis)不同年龄年表特征及其与气候因子间的关系,以期揭示年龄因素对年表的潜在影响。结果表明,平均年龄为63a的红松低龄年表与平均年龄为184a的高龄年表对气候的响应明显不同:低龄红松径向生长与当年1、2月月平均温度负相关(P<0.05),同时也受到上年及当年多个月份的月平均最高温度或最低温度的影响,但与降水的相关性未达到显著水平;高龄红松径向生长则与月平均温度间的关系不明显,而与当年1、2、4、6、7、9月的月平均最高温度正相关,与当年4月、9月的月平均最低温度负相关,同时受到上年5月及当年5月月总降水量的影响。因此,年龄因素对红松年表的气候响应方面存在一定影响,且高龄年表对气候响应的敏感性更高,包含有更多的气候信息。     

边缘效应带和保留带内红松幼林水分生态的差异

 以一个经过12年边缘效应带处理的14年生红松(Pinus koraiensis)(1998年)幼林生态系统为研究对象,对处于不同宽度的边缘效应带和保留带的红松幼树木质部水势、叶片蒸腾强度、气孔导度、叶片温度、空气相对湿度和光合有效辐射的日变化以及土壤相对含水量进行了分析,结合叶片净光合速率探讨了效应带宽度对红松幼林生态系统中红松幼树水分生态及红松生长状况的可能影响模式。结果表明：1）边缘效应带的开拓降低了效应带内红松幼树木质部水势、空气相对湿度和叶片气孔导度,显著提高了叶片蒸腾强度、叶片温度和光合有效辐射     

Moisture‐driven xylogenesis in Pinus ponderosa from a Mojave Desert mountain reveals high phenological plasticity

Future seasonal dynamics of wood formation in hyperarid environments are still unclear. Although temperature‐driven extension of the growing season and increased forest productivity are expected for boreal and temperate biomes under global warming, a similar trend remains questionable in water‐limited regions. We monitored cambial activity in a montane stand of ponderosa pine (Pinus ponderosa) from the Mojave Desert for 2 consecutive years (2015–2016) showing opposite‐sign anomalies between warm‐ and cold‐season precipitation. After the wet winter/spring of 2016, xylogenesis started 2 months earlier compared to 2015, characterized by abundant monsoonal (July–August) rainfall and hyperarid spring. Tree size did not influence the onset and ending of wood formation, highlighting a predominant climatic control over xylem phenological processes. Moisture conditions in the previous month, in particular soil water content and dew point, were the main drivers of cambial phenology. Latewood formation started roughly at the same time in both years; however, monsoonal precipitation triggered the formation of more false rings and density fluctuations in 2015. Because of uncertainties in future precipitation patterns simulated by global change models for the Southwestern United States, the dependency of P. ponderosa on seasonal moisture implies a greater conservation challenge than for species that respond mostly to temperature conditions.     

基于日均温度的华山松径向生长敏感温度研究

树干木质部形成周期与温度密切相关,存在影响形成层活动的敏感温度,但是尚未研究尝试从树木年轮中探索影响径向生长的敏感温度。华山主峰的华山松径向生长对气候变化较敏感,且华山西峰的气象站记录了1953年以来气象资料,这为探索树木径向生长与温度的关系提供了宝贵的材料。以华山主峰的华山松年轮资料和日值温度资料为基础,通过分析历年日平均温度的变化过程和年轮宽度、早材宽度、晚材宽度、最小密度以及最大密度的相关性,尝试探索华山松径向生长与日均温度变化的关系。结果表明春季一定温度的初日时间对华山松径向生长有较大的影响,其中3 ℃和8 ℃初日时间和持续时间对年轮宽度的促进作用最明显,而3 ℃对早材宽度影响较大,8℃初日时间对晚材的影响较大;高于11 ℃的温度会对华山松的径向生长造成限制,其中以11 ℃的作用最明显;而温度的终日时间对年轮特征影响较小。说明3 ℃是早材形成的敏感温度,8 ℃是晚材形成的敏感温度,温度高于11 ℃会对华山松的径向生长构成胁迫。这证明华山松年轮特征中包含了较多的气候信息,形成层活动和木质部的生长存在阈值温度,通过分析不同温度的生长期与年轮特征的关系可以找到影响华山松径向生长的敏感温度。这些敏感的温度是通过什么生理过程影响木质部的形成尚无法得知,但是这为解释树木生长对全球温度升高的响应以及利用华山松年轮重建历史气候提供了重要依据。     

Indole-3-Acetic Acid Controls Cambial Growth in Scots Pine by Positional Signaling

The vascular cambium produces secondary xylem and phloem in plants and is responsible for wood formation in forest trees. In this study we used a microscale mass-spectrometry technique coupled with cryosectioning to visualize the radial concentration gradient of endogenous indole-3-acetic acid (IAA) across the cambial meristem and the differentiating derivatives in Scots pine (Pinus sylvestris L.) trees that had different rates of cambial growth. This approach allowed us to investigate the relationship between growth rate and the concentration of endogenous IAA in the dividing cells. We also tested the hypothesis that IAA is a positional signal in xylem development (C. Uggla, T. Moritz, G. Sandberg, B. Sundberg [1996] Proc Natl Acad Sci USA 93: 9282–9286). This idea postulates that the width of the radial concentration gradient of IAA regulates the radial number of dividing cells in the cambial meristem, which is an important component for determining cambial growth rate. The relationship between IAA concentration in the dividing cells and growth rate was poor, although the highest IAA concentration was observed in the fastest-growing cambia. The radial width of the IAA concentration gradient showed a strong correlation with cambial growth rate. The results indicate that IAA gives positional information in plants.     

Ascorbic acid and development of xylem and phloem cells in the pine trunk

Changes in the levels of ascorbic acid (AA), its oxidized form, dehydroascorbic acid (DHA), and uronic acids as initial precursors for the AA synthesis were studied as related to the degree of xylem and phloem cell development in the course of early and late wood formation in the trunks of Scots pine (Pinus sylvestris L.). The cells of mature and conducting phloem, cambial zone, differently developed cells in the zones of cell enlargement and maturation were obtained by successive scraping tissue layers from trunk segments of 20–25-year-old trees; tissue identification was checked anatomically and histochemically. The contents of compounds tested were calculated per dry weight and per cell basis. We found great differences in the contents of AA and DHA and also in their ratio in dependence of the wood type developing in the pine trunks during growth period and on the stage of differentiation of xylem and phloem cells. Changes in the AA content during xylem cell differentiation were accompanied by changes in the content of uronic acids. The amounts of AA, DHA, and uronic acids were the highest at the stage of early lignification and reduced with tracheid maturation. The AA to DHA ratio changed differently in the course of early and late xylem lignification. It reduced from the start of lignification to the formation of early mature xylem and, in contrast, increased in mature late wood; this indicates a difference in the level of redox processes in these tissues.     

Fluctuations of cambial activity in relation to precipitation result in annual rings and intra-annual growth zones of xylem and phloem in teak (Tectona grandis) in Ivory Coast

Background and Aims Teak forms xylem rings that potentially carry records of carbon sequestration and climate in the tropics. These records are only useful when the structural variations of tree rings and their periodicity of formation are known. Methods The seasonality of ring formation in mature teak trees was examined via correlative analysis of cambial activity, xylem and phloem formation, and climate throughout 1·5 years. Xylem and phloem differentiation were visualized by light microscopy and scanning electron microscopy. Key Results A 3 month dry season resulted in semi-deciduousness, cambial dormancy and formation of annual xylem growth rings (AXGRs). Intra-annual xylem and phloem growth was characterized by variable intensity. Morphometric features of cambium such as cambium thickness and differentiating xylem layers were positively correlated. Cambium thickness was strongly correlated with monthly rainfall (R(2) = 0·7535). In all sampled trees, xylem growth zones (XGZs) were formed within the AXGRs during the seasonal development of new foliage. When trees achieved full leaf, the xylem in the new XGZs appeared completely differentiated and functional for water transport. Two phloem growth rings were formed in one growing season. Conclusions The seasonal formation pattern and microstructure of teak xylem suggest that AXGRs and XGZs can be used as proxies for analyses of the tree history and climate at annual and intra-annual resolution.     

Cambial activity and annual rhythm of xylem production of Pinus kesiya Royle ex. Gordon (Pinaceae) in relation to phenology and climatic factors growing in sub-tropical wet forest of North East India

The interrelationship between phenological events, climatic factors, periodicity of cambial activity and seasonal production of xylem was examined in Pinus kesiya Royle ex. Gordon growing in sub-tropical wet forest of Meghalaya state, India. Reactivation of dormant cambium occurs after sprouting of new needles during the middle of February. Since the formation of reproductive cones takes place simultaneously with vegetative bud break and needle formation, cone formation could also lead to the enhancement of cambial activity. The activity of cambium and xylem production decline gradually towards November and cease from end of December to end of January. There was no correlation between needle fall and cambial activity. Due to the production of three flushes of new needles and branches in a year the tree never becomes completely leafless. It was evident from correlation and regression analysis that the annual course of average temperature plays an important role for the reactivation of vascular cambium after dormancy. The differentiation of xylem elements correlated with mean temperature in the first place and secondly with precipitation. Increase in length of fusiform initials and their derivatives could be correlated with relative humidity, precipitation and mean maximum temperature. Dormancy was imposed by low temperature and less precipitation. The data are discussed in the light of cambial activity, xylem production and phenological events.     

Growth Regulators and Wood Formation in Pinus silvestris

The formation of new xylem in the spring is preceded by bud development. In decapitated pine stem the formation of xylem is arrested until the outgrowth of interfascicular buds takes place. When indole-3yl-acetic acid (IAA) is applied to the cut surfaces of decapitated stems it induces the formation of a xylem ring on the whole length of 5-ycar old trees. Naphthaleneacetic acid (NAA) causes the formation of xylem; however, the width of the growth ring is several times broader at the point of application than at the base of the leader. Cis- and trans-cinnamic acids, coumarin, L-tryptophan, kinetin (Kin), benzylaminopurine (BAP) and gibberellic acid (GA) alone do not induce cambial divisions; however, GA and the cytokinins given jointly with IAA or NAA accelerated the basipetal stimulus which has been induced by the auxins, resulting in normal xylem formation. 2,3,5-Triiodobonzoic acid (TIBA) given jointly with IAA-induced formation of compression wood in the apical part of the stem and narrow diameter tracheids at the base. When carboxyl labelled IAA or NAA are applied to pine segments it is found that the basipetal movement of IAA is much quicker than that of NAA. GA and the cytokinins increase the rate of transport of both auxins, whereas TIBA arrests the bulk of auxin in the apical part of the stem.     

Adjustment Capacity of Maritime Pine Cambial Activity in Drought-Prone Environments

Intra-annual density fluctuations (IADFs) are anatomical features formed in response to changes in the environmental conditions within the growing season. These anatomical features are commonly observed in Mediterranean pines, being more frequent in younger and wider tree rings. However, the process behind IADF formation is still unknown. Weekly monitoring of cambial activity and wood formation would fill this void. Although studies describing cambial activity and wood formation have become frequent, this knowledge is still fragmentary in the Mediterranean region. Here we present data from the monitoring of cambial activity and wood formation in two diameter classes of maritime pine (Pinus pinaster Ait.), over two years, in order to test: (i) whether the differences in stem diameter in an even-aged stand were due to timings and/or rates of xylogenesis; (ii) if IADFs were more common in large trees; and (iii) if their formation is triggered by cambial resumption after the summer drought. Larger trees showed higher rates of cell production and longer growing seasons, due to an earlier start and later end of xylogenesis. When a drier winter occurs, larger trees were more affected, probably limiting xylogenesis in the summer months. In both diameter classes a latewood IADF was formed in 2012 in response to late-September precipitation, confirming that the timing of the precipitation event after the summer drought is crucial in determining the resumption of cambial activity and whether or not an IADF is formed. It was the first time that the formation of a latewood IADF was monitored at a weekly time scale in maritime pine. The capacity of maritime pine to adjust cambial activity to the current environmental conditions represents a valuable strategy under the future climate change conditions.     

Periodicity of Wood Formation in Some Trees of Lowland Rainforest in Nigeria

Freshly prepared chlor-zinc-iodide was used to determine theperiodicity of wood formation at breast height (144 cm fromthe ground) in the trunks of some trees growing in the LowlandRainforest around Ibadan, Nigeria. Wood formation shows seasonal periodicity in the plants studied.The cambial derivates on the xylem side differentiate into woodcells, which at a certain stage of differentiation have abundantcellulose in their secondary walls. The cellulose stains deepblue in chlor-zinc-iodide. This has been used as a criterionfor deciding that wood formation has started. When no cellswith deep blue staining secondary walls are found the cambiumis known to be dormant or quiscent. The resumption of cambial activity is correlated positivelywith bud break and unfolding of new leaves. In Bombax buonopozenseP. Beauv. the relationship may be obscured by local cambialactivity induced by injury. Wood formation stops in the trunks either towards the end ofthe rainy season or at the early part of the dry season. Itstarts either during the dry season or at the beginning of therainy season; but the bulk of the wood is formed during therainy season. Cambial activity stops in most cases before leaffall. At the cessation of wood formation the fully lignifiedxylem elements abut on the xylem mother cells or on xylem cellswith incompletely thickened cell walls. Presence or absence of a starch-free-zone and the noding ofthe vascular rays also give indications of seasonal periodicityin wood formation. Growth rings are periodic and one growthring is generally formed each year.     

阔叶红松林净初级生产力模型参数的敏感性

PnET-Ⅱ(photosynthesis and evapotranspiration)模型是生态系统过程模型,运行过程中所需的参数较多, 包括植被、土壤和气候参数等.本文估计了丰林自然保护区阔叶红松林中红松和阔叶树的总净初级生产力（NPP）和枝干NPP对PnET-Ⅱ模型参数变化的敏感程度.结果表明: PnET-Ⅱ模型的植被参数中,林冠参数变化对模拟结果影响较大,且红松总NPP对植被参数的敏感性大于阔叶树;红松和阔叶树NPP对土壤持水量变化敏感性较小,且红松NPP对土壤持水量的敏感性略小于阔叶树;在气候情景范围内,气温变化对红松和阔叶树NPP的影响最大,降水和光合有效辐射次之.不同气候情景对NPP模拟结果的影响不同.红松和阔叶树的总NPP和枝干NPP对各输入参数的敏感程度并不完全一致.     

Seasonal development of secondary xylem and phloem in <Emphasis Type="Italic">Schizolobium parahyba</Emphasis> (Vell.) Blake (Leguminosae: Caesalpinioideae)

The cambial activity and periodicity of secondary xylem and phloem formation have been less studied in tropical tree species than in temperate ones. This paper describes the relationship between seasonal cambial activity, xylem and phloem development, and phenology in Schizolobium parahyba, a fast growing semideciduous seasonal forest tree from southeastern Brazil. From 2002 to 2003, wood samples were collected periodically and phenology and climate were recorded monthly in the same period. S. parahyba forms annual growth increments in wood, delimited by narrow initial parenchyma bands. The reduction of the cambial activity to a minimum correlates to the dry season and leaf fall. The higher cambial activity correlates to the wet season and the presence of mature leaves. In phloem, a larger conductive region was observed in the wet season, when the trees were in full foliage. The secondary phloem did not exhibit any incremental zone marker; however, we found that the axial parenchyma tends to form irregular bands.     

The effects of artificial soil frost on cambial activity and xylem formation in Norway spruce

We studied the effects of artificial soil frost on cambial activity and xylem formation on 47-year-old Norway spruce [Picea abies (L.) Karst.] trees grown on medium fertile site type (with moraine soil) in eastern Finland (62°42′N; 29°45′E). Different soil frost treatments applied were: (1) natural snow accumulation and melting (control, CTRL); (2) artificial removal of snow from soil surface during two consecutive winters (OPEN); and (3) snow clearing and insulation (FROST), which was in other ways similar to OPEN, but the ground was insulated in early spring to delay soil thawing. Each treatment was replicated in three blocks, and two sample trees in each plot were repeatedly microcored during growing seasons of 2006–2007 for the analysis of the onset, cessation and the duration of xylem formation. The phases of tracheid differentiation (tracheids in radial enlargement, secondary cell wall formation, and mature tracheids) were measured from the microcores of 2007. The intra-ring growth and wood density variables were analysed based on X-ray densitometry. In FROST in 2006, xylem formation started a week later than in the other treatments. In 2007, no difference was found between the treatments. The discrepancy in results between the two study years may be explained by between-years variation in weather, i.e., the winter was colder in 2005/2006 than in 2006/2007. No effects of soil frost treatments on tracheid differentiation and on most of the intra-ring growth and density variables were discovered. Our results suggest that the delayed thawing of moraine soil may slightly affect the onset, timing and duration of xylem formation in Norway spruce. However, the effects of delayed soil frost may depend also on the soil type and become more evident with increasing water holding capacity of the soil.     

西双版纳楝径向生长和木质部发生季节动态及其对环境因子的响应

热带森林在全球碳循环过程中起着重要的作用,研究热带树木的生长动态及其对环境因子的响应,有助于预测全球变化下热带森林固碳能力的变化。目前对热带树木径向生长以及木质部发生季节动态的研究相对较少。利用微树芯和生长环法对西双版纳热带植物园内的落叶树种楝(Melia azedarach)2021年的年内径向生长和木质部发生季节动态进行监测,结合环境因子的监测,分析了楝的径向生长过程的驱动因子。结果表明：2021年楝的扩大细胞在3月1日(年积日(DOY):60.2±1.6)开始出现,细胞壁加厚在12月11日(DOY:345.4±3.1)结束,年生长量为7.76 mm,最大生长速率为0.039 mm/d。生长环监测显示,楝在3月18日(DOY:76.6±8.6)左右开始生长,10月13日(DOY:286.4±6.8)生长结束,年径向生长量为(6.25±2.35)mm,最大生长速率为(0.056±0.02)mm/d。楝的径向生长速率与降水(r=0.77,P<0.001)、平均温度(r=0.61,P<0.05)和最低温度(r=0.67,P<0.001)均呈显著正相关,与风速(r=-0....