蒂瓦共和国西部坦努奥拉山脉雪松林边界的状态和动态

KH.B. KUULAR
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摘要

本文介绍了西坦努-奥拉山脉森林中暗针叶林和雪松林下对该地区观测到的气候变化的近期响应。根据附近察丹气象站资料,年平均气温异常值为1.6±0.8°С,生长期异常值为1.0±0.7°С。重点研究区域位于泰瓦共和国境内,北纬50°55′-51°15′,东经91°30′-92°20′之间,对应三个海拔高度:与草原接壤的中山下带(海拔1100-1300米),覆盖着落叶松和桦树林;中部山脉的中部地带(海拔1300-1800米),被落叶松和雪松林覆盖;中部山脉上带的落叶松和雪松林(海拔1800-2120米)。在田间工作过程中,测定了杉木树苗顶梢的生长量,以及树龄、树高和总树数。利用察丹气象站多年的观测资料,定量地确定了增量、气温和相对湿度之间的相关性。结果表明:山腰下部的湿度与山腰上部的气温呈正相关;中部山区下部和中部山区上部杉木树苗数量的增加,证实了在区域气候变暖的影响下,暗针叶林在山脊上下移动。Landsat TM/ETM+/OLI空间影像显示NDVI和NDWI植被指数呈增加趋势。根据卫星图像,计算了过去几十年来重点地区暗针叶林面积的增加;然而,这些数据的可靠性没有进行统计评估。这项工作需要在实地继续进行。
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THE STATE AND DYNAMICS OF THE BORDERS OF CEDAR FORESTS AT THE WESTERN TANNU-OLA RANGE IN THE TYVA REPUBLIC
The paper presents the recent response of dark coniferous forest and cedar undergrowth in the forests of the Western Tannu-Ola Range to the observed climate change in the region. According to the nearby Chadan meteorological station, the anomaly of the average annual air temperature was 1,6 ± 0,8°С, the anomaly of the growing season was 1,0 ± 0,7°С. Key study areas are located in the Tyva Republic within 50°55′-51°15′N and 91°30’-92°20’E, which corresponds to three altitudinal levels: the lower belt of the middle mountains (1100-1300 m a.s.l.) bordering the steppe and covered with larch forests with birch; the middle belt of the middle mountains (1300-1800 m a.s.l.) covered with larch and cedar forests; larch and cedar forests of the upper belt of the middle mountains (1800-2120 m a.s.l.). In the course of field work, the increment of the top shoot of cedar sapling (Pinus sibirica Du Tour) was measured, as well as its height, age and total number. Correlations between the increment, air temperature and relative humidity were quantitatively determined using data from the Chadan weather station for a number of years. The results indicate a positive correlation with humidity in the lower zone of the middle mountains and with air temperature in the upper zone of the middle mountains. Higher amounts of cedar sapling in the lower zone of the middle mountains and in the upper zone of the middle mountains confirm the shift of dark coniferous forests down and up the ridge under the regional climate warming. Space images of Landsat TM/ETM+/OLI show the increasing values of NDVI and NDWI vegetation indices. According to satellite images, an increase in the area of dark coniferous forests over the past decades was calculated for the territory of key areas; however, the reliability of these data was not evaluated statistically. The work needs to be continued in the field.
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