地理研究 ›› 2019, Vol. 38 ›› Issue (4): 807-821.doi: 10.11821/dlyj020180111
收稿日期:
2018-01-25
修回日期:
2018-03-23
出版日期:
2019-04-20
发布日期:
2019-04-20
作者简介:
作者简介:王晓利(1985-),女,四川广元人,博士,助理研究员,主要从事海岸带气候变化与生态风险评估研究。E-mail:
基金资助:
Xiaoli WANG1,2(), Xiyong HOU1,2(
)
Received:
2018-01-25
Revised:
2018-03-23
Online:
2019-04-20
Published:
2019-04-20
摘要:
基于1982—2014年GIMMS NDVI3g数据集,分析中国沿海地区生长季归一化植被指数(NDVI)的时空变化特征,探讨NDVI对极端气温和极端降水年尺度和月尺度的响应特征。结果表明:中国沿海地区及其子区域NDVI均呈上升趋势,且该趋势具有一定持续性;江南及其以南各子区域的NDVI高于江南以北,但长江三角洲、珠江三角洲等地区NDVI下降较明显,而江南以北沿海地区NDVI多呈上升趋势。NDVI在东北沿海西部、华北和黄淮沿海各子区域与极端气温暖指数(暖昼日数和日最高气温的极高值)多呈负相关,在其他沿海地区多呈正相关。NDVI与极端气温冷指数(冷昼日数和日最低气温的极低值)在整个沿海地区基本呈负相关,且对冷指数的响应具有一定滞后性;江淮(含)以南各子区域的NDVI与气温日较差多呈正相关,以北基本呈负相关。NDVI在黄淮以北与极端降水之间一般呈正相关,在黄淮(含)以南和东北沿海中东部地区多呈负相关,黄淮(含)以北各子区域的NDVI对极端降水的滞后效应较明显。
王晓利, 侯西勇. 1982—2014年中国沿海地区归一化植被指数(NDVI)变化及其对极端气候的响应[J]. 地理研究, 2019, 38(4): 807-821.
Xiaoli WANG, Xiyong HOU. Variation of Normalized Difference Vegetation Index and its response to extreme climate in coastal China during 1982-2014[J]. GEOGRAPHICAL RESEARCH, 2019, 38(4): 807-821.
表1
气候指数的定义与分类"
分类 | 代码 | 名称 | 定义 | 单位 |
---|---|---|---|---|
气温类指数 | TX10p | 冷昼日数 | 日最高气温<10%分位值的日数 | d |
TX90p | 暖昼日数 | 日最高气温>90%分位值的日数 | d | |
DTR | 气温日较差 | 年内日最高气温与最低气温的差值 | oC | |
TXx | 日最高气温的极高值 | 每月内日最高气温的最大值 | oC | |
TNn | 日最低气温的极低值 | 每月内日最低气温的最小值 | oC | |
Tm | 月平均气温 | 每月所有日数的平均气温 | oC | |
Ty | 年平均气温 | 每年所有月份的平均气温 | oC | |
降水类指数 | RX1day | 单日最大降水量 | 每月最大1日降水量 | mm |
RX5day | 连续5日最大降水量 | 每月连续5日最大降水量 | mm | |
TPm | 月降水量 | 每月所有降水日数的总降水量 | mm | |
TPy | 年降水量 | 全年所有降水日数的总降水量 | mm |
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