地球信息科学学报 ›› 2019, Vol. 21 ›› Issue (6): 958-968.doi: 10.12082/dqxxkx.2019.180686
收稿日期:
2018-12-27
修回日期:
2019-02-22
出版日期:
2019-06-15
发布日期:
2019-06-15
作者简介:
作者简介:左冰洁(1993-),女,湖北武汉人,硕士生,主要从事森林资源监测与评价研究。E-mail:
基金资助:
Received:
2018-12-27
Revised:
2019-02-22
Online:
2019-06-15
Published:
2019-06-15
Contact:
Yujun SUN
Supported by:
摘要:
在全球气候变化背景下,植被动态变化以及植被对气候变化的响应方式已经成为生态学和地理学领域的热点。本文对比分析了南方亚热带季风区将乐县不同类型森林植被对不同时间尺度的干旱响应的差别。基于2000-2017年MODIS-EVI数据及气象站点数据,用最大值合成法、趋势分析法以及相关分析法,分析了森林植被及气象因子的动态变化特征,并对比不同森林植被对气候变化响应的差别。研究表明:① 2000-2017年,研究区植被覆盖度、EVI和降水均显著增加,区域内湿度增加,森林长势渐趋良好;② EVI在生长季初期和末期与同期的降水、温度均显著正相关(P<0.1),初期森林受降水因子的影响更大,末期受温度因子的影响大;③ 1-3月和周年的气候变化对森林的生长至关重要,长时间尺度的湿度增加对森林生长具有显著的促进作用,SPEI的时间尺度越长与EVI的相关性也越大;④ 针阔混交林与同期温度、降水的相关系数最高,并且与不同时间尺度的SPEI相关性均比较高,属于气候敏感型林型,在生产经营中要谨慎预防气候变化对该林型带来的伤害;⑤ 森林覆盖度变化与降水和SPEI_24的相关性极显著,长时间尺度的降水变化是影响森林植被覆盖率变化的重要因素之一。
左冰洁, 孙玉军. 南方亚热带季风区将乐县森林植被动态变化及其对气候变化的响应[J]. 地球信息科学学报, 2019, 21(6): 958-968.DOI:10.12082/dqxxkx.2019.180686
Bingjie ZUO, Yujun SUN. Forest Vegetation Dynamics and Responses to Climate Change in a Southern Subtropical Monsoon Region in Jangle County[J]. Journal of Geo-information Science, 2019, 21(6): 958-968.DOI:10.12082/dqxxkx.2019.180686
表2
2000-2017年将乐县生长季不同森林植被EVI与降水和温度偏相关系数
月份 | 类别 | 阔叶林 | 针阔混交林 | 针叶林 | 竹林 |
---|---|---|---|---|---|
3 | 温度 | 0.242 | 0.302* | 0.3* | 0.277* |
降水 | 0.452** | 0.438** | 0.438** | 0.494** | |
4 | 温度 | 0.165 | 0.160 | 0.15 | 0.173 |
降水 | -0.235 | -0.254 | -0.247 | -0.232 | |
5 | 温度 | -0.354* | -0.38* | -0.325* | -0.354* |
降水 | -0.307* | -0.37* | -0.325* | -0.335* | |
6 | 温度 | 0.419** | 0.366* | 0.384* | 0.393* |
降水 | -0.185 | -0.093 | -0.112 | -0.162 | |
7 | 温度 | -0.037 | -0.031 | 0.006 | -0.035 |
降水 | 0.053 | 0.145 | 0.169 | 0.032 | |
8 | 温度 | 0.043 | -0.102 | -0.019 | 0.039 |
降水 | -0.084 | -0.103 | -0.033 | -0.1 | |
9 | 温度 | 0.362* | 0.361* | 0.347* | 0.374* |
降水 | 0.286* | 0.307* | 0.343* | 0.294* |
表3
2000-2017年将乐县生长季不同森林植被EVI对SPEI最大响应的时间尺度
月份 | 阔叶林 | 针叶林 | 针阔混交林 | 竹林 |
---|---|---|---|---|
3 | 1(0.390*) | 1(0.354*) | 1(0.328*) | 1(0.421**) |
4 | 3(-0.376*) | 3(-0.377*) | 3(-0.404*) | 3(0.389*) |
5 | 21(0.410**) | 21(0.447**) | 21(0.391*) | 21(0.403*) |
6 | 1(-0.283) | 1(-0.196) | 1(-0.183) | 1(-0.260) |
7 | 24(0.575***) | 24(0.606***) | 24(0.608***) | 24(0.534***) |
8 | 21(0.377*) | 12(0.361*) | 12(0.342*) | 15(0.395*) |
9 | 4(-0.207) | 4(-0.147) | 3(0.129) | 4(-0.193) |
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