924 resultados para Tree-rings


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本文研究了木本植物的不同部位即叶片、枝条和树皮以及植物的生理指标如气孔阻力对大气S02、TSP和重金属污染的指示和监测作用,并用树木年轮指示大气污染的历史和程度。结果认为: 承德市大气污染自1703年城市化以来开始出现,但达到严重污染水平则出现在本世纪50年代以来尤其是最近10-20年城市化与工业化的加剧,主要污染物以S02为主,从避暑山庄修建前的<0.1μg m-3达到目前的30μg m-3,重金属污染Fe自1927-45大庙铁矿开采后出现,Mn、Ni、Pb等出现在工业化以来的最近40-50年中,上述污染物含量在木质部年轮中明显升高,如S增加了10倍以上,Pb增加了560% (P<0.00l)。 不同城市功能区树皮pH和气孔阻力不同,主要与大气中的S02和TSP有关,据此可监测大气S02和TSP污染。前者以榆树、加拿大杨、垂柳和国槐最佳,相关系数分别可达-0.8384 (P<0.0l),-0.7447、-0.6904和-0.6552 (P<0.05);后者则以白腊和旱柳下表皮最好,相关系数达0.9968和0.9951 (P<0.00l)。在扫描电镜下发现气孔受大气TSP影响出现不同程度的堵塞现象,主要有2种途径,小型颗粒物(<5μm)进入气孔腔,大型颗粒物(>30μm)可将气孔封盖。 植物不同器官部位污染物含量以树皮为最高,其次是枝条或叶,因而适宜的指示或监测部位是叶或枝条。主分量分析认为:承德市大气污染物以S为主,重金属Fe、Zn、Mn也有一定的贡献,Pb仅出现在繁忙道路区。不同季节污染物含量变化以休眠期最高,生长初期次之,生长旺盛期最低,如S和Pb分别从0.75 mg g-1和0.7 mg g-1上升到1.5 mg g-1和2.0 mg g-1(P<0.001)。植物不同季节污染物含量的变化反应了大气污染物季节变化特点,因而可以指示或监测大气污染尤其是S02污染。其中刺槐多部位复相关模型监测效果最佳,复相关系数可达0.987;某些植物单一部位的监测作用也较好,叶以珍珠梅最佳,相关系数为0.8695 (P<0.001),枝以油松、珍珠梅、垂柳为好(r≥0.8,P <0.001),树皮以刺槐为佳,r=0.8615 (P<0.0l)。植物不同部位的污染物含量还可用来评价大气环境质量,其中复合污染指数可以 评价总的大气环境质量,S污染指数和重金属污染指数可以评价S02、重金属和TSP污染,与直接利用污染物浓度法基本一致。油松不同部位对于大气S02的指示作用可表现为年轮对大气污染历史的指示或监测,针叶对现状S02污染的预测,并利用针叶对于S02的监测结果,绘制了大气S02污染分布图。 总之,本文利用古松年轮和现状城市植物的枝条、叶和树皮中的污染物含量以及树皮酸度等不同方面的指标,对承德市大气污染的历史和现状进行了指示与监测,即承德市大气污染从过去到现在均以S02为主,植物不同部位可以非常有效地进行大气S02污染的监测与评价,其中多部位的复相关模型预测效果极佳。另外,由植物监测而绘制的大气S02分布图,较准确地揭示了承德市大气S02现状分布规律。

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EXTRACT (SEE PDF FOR FULL ABSTRACT): Tree-ring records from foxtail pine (Pinus balfouriana) and western juniper (Juniperus occidentalis) growing near tree line in the eastern Sierra Nevada, California, show strong correlations with summer temperature and winter precipitation. Response surfaces portraying tree growth as a function of summer temperature and winter precipitation indicate a strong interaction between these variables in controlling growth. ... Above average growth for both foxtail pine and western juniper from AD 1480 to 1570 can be interpreted as indicating an extended period of warm, moist conditions unequalled during the 20th century.

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Cross-spectral analysis of regional tree-ring data suggests the spatial pattern of correlation between moisture variations in the Sierra Nevada of central California and in other parts of the western United States is frequency dependent. Short wavelengths (2.8 to 10.7 years), perhaps associated with El Niño/Southern Oscillation, are strongly coherent both to the north (Oregon) and to the south (Southern California). Longer wavelengths (45 to 75 years) are strongly coherent only to the north. Frequency bands corresponding to annual sunspot series were associated with relatively weak patterns of spatial correlation.

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Climate conditions in land areas of the Pacific Northwest are strongly influenced by atmosphere/ocean variability, including fluctuations in the Aleutian Low, Pacific-North American (PNA) atmospheric circulation modes, and the El Niño-Southern Oscillation (ENSO). It thus seems likely that climatically sensitive tree-ring data from these coastal land areas would likewise reflect such climatic parameters. In this paper, tree-ring width and maximum lakewood density chronologies from northwestern Washington State and near Vancouver Island, British Columbia, are compared to surface air temperature and precipitation from nearby coastal and near-coastal land stations and to monthly sea surface temperature (SST) and sea level pressure (SLP) data from the northeast Pacific sector. Results show much promise for eventual reconstruction of these parameters, potentially extending available instrumental records for the northeastern Pacific by several hundred years or more.

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EXTRACT (SEE PDF FOR FULL ABSTRACT): In this work, I examine patterns of atmospheric circulation associated with tree growth anomalies at mid-to-high latitudes (2000-3500 meters).

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A key to understanding the causes for climate variability lies in understanding how atmospheric circulation influences regional climate. The goal of this research is to investigate the long-term relationships between atmospheric circulation and winter climate in the southwestern United States. Patterns of atmospheric circulation are described by circulation indices, and winter climate is defined as number of days with precipitation and mean maximum temperature for the winter wet season, November through March. Records of both circulation indices and climate variables were reconstructed with tree-ring chronologies for the period 1702-1983. The years of the highest and lowest values of circulation indices and climate variables were compared in order to investigate possible spatial and temporal relationships between extremes in circulation and climate.