气候改变对斯里兰卡茶产业的影响外文翻译(节选)
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1、1860 单词, 2628 汉字 出处: Wijeratne M A. Vulnerability of Sri Lanka tea production to global climate changeJ. Water Air & Soil Pollution, 1996, 92(1-2):87-94. 原文 VULNERABILITY OF SRI LANKA TEA PRODUCTION TO GLOBAL CLIMATE CHANGE M.A. WIJERATNE Introduction Although industrial exports such as textiles and
2、 garments bring in a higher percentage of foreign exchange, agriculture is the highest net foreign exchange earner in Sri Lanka. Of the agricultural exports, tea alone contributes about 15-25% of the total exchange earnings and, hence, plays a key role in the Sri Lankan economy. About 30% of the emp
3、loyees of the public sector government and semigovernment are manual workers on estates, and the majority of these are employed on tea plantations. Moreover, about 239,000 tea small holdings also generate a large proportion of employment opportunities in the country. Accordingly, more than 700,000 w
4、orkers and their families are dependent on the tea industry. These figures show the importance of the tea industry to the social and economic stability of Sri Lanka In spite of the expansion of the small holdings sector, in Sri Lanka, the total area of tea plantations has decreased since the 1930s,
5、i.e., from about 0.44 to 0.23 x 10 s ha. The decline in the estate sector tea lands began early in the 1960s, because of low productivity brought about by soil and bush debilitation. Many of the midcountry 600-1,200 m elevation tea plantations have now become marginal, warranting crop diversificatio
6、n. Adversities of weather and poor management practices have been blamed for this situation; changes in the microclimate in tea plantations after shade removal during the early 1960s have also affected the productivity of the tea bushes Fuch, 1989. Some adverse effects of the nationalization of the
7、plantations in the 1970s, such as the neglect of agricultural practices, contributed to the decline in the estate sector production Fuch, 1989. Being a rainfed plantation crop in Sri Lanka, tea depends greatly on weather for optimal growth. Therefore, changes in weather conditions would undoubtedly
8、affect tea production. The relationship between tea yield and weather has been discussed by many researchers e.g., Devanathan, 1975; Kandiah and Thevadasan, 1980; Carr and Stephens, 1992. The findings of this study differ from those of the Sri Lanka country report ADB, 1994. This could be due to the
9、 different models used to predict tea yield. It is generally accepted that an increase in temperature increases tea yield, and this relationship has been used in many models. But recent findings show that at higher temperature regimes greater than 25-26 C, the increase in temperatures reduces tea yi
10、eld . Droughts inflict irreparable losses to the tea industry and hence to the economy of Sri Lanka. The consequences of the droughts in 1983 and 1992 are good examples Central Bank, 1983; 1992. The decline in production due to drought in early 1983 was about 4% over the previous year, and the droug
11、ht in 1992 reduced tea production by about 26% compared to that of 1991. It also increased the costs of production by 19%, depriving the country of about 3 billion rupees US$70 million of foreign exchange. Total production in 1991 and 1992 was 240.7 and 178.9 10 kg, respectively, and the latter was
12、the lowest production recorded since the end of the 1950s Figure 1. These figures show the magnitude of the loss that could be incurred by adversities of weather Heavy rainfall also causes considerable damage to tea plantations through soil erosion, poor growth due to lack of sun, and increases in d
13、isease incidence. Poorly covered old seedling tea fields, pruned tea fields, and young tea fields during the first two years are more vulnerable to soil erosion due to inadequate ground cover. It has been estimated that more than 30 cm of top soil has already been lost from Sri Lankas tea plantation
14、s, especially in the uplands Krishnaraj ah, 1985. Landslides also adversely affect plantations and endanger the lives of workers on the hilly slopes. Climate Change and Methods According to climate change scenarios, the increases in global atmospheric CO 2 concentrations and temperatures by 2100 cou
15、ld be in the range of 600-700 ppm and 1.0-3.5 C, respectively, compared to 1990, depending on different scenarios of variations in greenhouse gas emissions CO2, CH4, N20 and oceanic changes Houghton et al., 1996The consequences of climate change will differ from one country to another. In the recent
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