Ecology and Environment ›› 2021, Vol. 30 ›› Issue (12): 2285-2293.DOI: 10.16258/j.cnki.1674-5906.2021.12.002
• Research Articles • Previous Articles Next Articles
MA Bingxin1(), JING Juanli1,2, XU Yong1,*(
), HE Hongchang1, LIU Bing1
Received:
2021-07-22
Online:
2021-12-18
Published:
2022-01-04
Contact:
XU Yong
马炳鑫1(), 靖娟利1,2, 徐勇1,*(
), 何宏昌1, 刘兵1
通讯作者:
徐勇
作者简介:
马炳鑫(1996年生),男,硕士研究生,研究方向为生态遥感。E-mail: 1654397198@qq.com
基金资助:
CLC Number:
MA Bingxin, JING Juanli, XU Yong, HE Hongchang, LIU Bing. Spatial-Temporal Changes of NPP and Its Relationship with Climate Change in Karst Areas of Yunnan, Guizhou and Guangxi from 2000 to 2019[J]. Ecology and Environment, 2021, 30(12): 2285-2293.
马炳鑫, 靖娟利, 徐勇, 何宏昌, 刘兵. 2000—2019年滇黔桂岩溶区植被NPP时空变化及与气候变化的关系研究[J]. 生态环境学报, 2021, 30(12): 2285-2293.
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URL: https://www.jeesci.com/EN/10.16258/j.cnki.1674-5906.2021.12.002
变化类型 Change type | 判断依据 Judgment based | 面积占比 Area proportion/% |
---|---|---|
显著增加 | S>0, |Z|>1.96 | 46.61 |
不显著增加 | S>0, |Z|<1.96 | 33.58 |
显著减少 | S<0, |Z|>1.96 | 15.13 |
不显著减少 | S<0, |Z|<1.96 | 4.68 |
Table 1 Change trend of NPP in karst areas of Yunnan, Guizhou and Guangxi
变化类型 Change type | 判断依据 Judgment based | 面积占比 Area proportion/% |
---|---|---|
显著增加 | S>0, |Z|>1.96 | 46.61 |
不显著增加 | S>0, |Z|<1.96 | 33.58 |
显著减少 | S<0, |Z|>1.96 | 15.13 |
不显著减少 | S<0, |Z|<1.96 | 4.68 |
变化类型 Change type | 判断依据 Judgment based | 面积占比 Area proportion/% |
---|---|---|
1. 强持续显著增加 | S>0, |Z|>1.96, H>0.75 | 33.03 |
2. 强持续不显著增加 | S>0, |Z|<1.96, H>0.75 | 8.20 |
3. 弱持续显著增加 | S>0, |Z|>1.96, 0.5<H<0.75 | 13.27 |
4. 弱持续不显著增加 | S>0, |Z|<1.96, 0.5<H<0.75 | 22.86 |
5. 反持续显著减少 | S<0, |Z|>1.96, H<0.5 | 0.01 |
6. 反持续不显著减少 | S<0, |Z|<1.96, H<0.5 | 1.16 |
7. 反持续不显著增加 | S>0, |Z|<1.96, H<0.5 | 2.65 |
8. 反持续显著增加 | S>0, |Z|>1.96, H<0.5 | 0.09 |
9. 弱持续不显著减少 | S<0, |Z|<1.96, 0.5<H<0.75 | 8.27 |
10. 弱持续显著减少 | S<0, |Z|>1.96, 0.5<H<0.75 | 0.72 |
11. 强持续不显著减少 | S<0, |Z|<1.96, H>0.75 | 5.77 |
12. 强持续显著减少 | S<0, |Z|>1.96, H>0.75 | 3.97 |
Table 2 Future change trend of NPP in karst areas of Yunnan, Guizhou and Guangxi
变化类型 Change type | 判断依据 Judgment based | 面积占比 Area proportion/% |
---|---|---|
1. 强持续显著增加 | S>0, |Z|>1.96, H>0.75 | 33.03 |
2. 强持续不显著增加 | S>0, |Z|<1.96, H>0.75 | 8.20 |
3. 弱持续显著增加 | S>0, |Z|>1.96, 0.5<H<0.75 | 13.27 |
4. 弱持续不显著增加 | S>0, |Z|<1.96, 0.5<H<0.75 | 22.86 |
5. 反持续显著减少 | S<0, |Z|>1.96, H<0.5 | 0.01 |
6. 反持续不显著减少 | S<0, |Z|<1.96, H<0.5 | 1.16 |
7. 反持续不显著增加 | S>0, |Z|<1.96, H<0.5 | 2.65 |
8. 反持续显著增加 | S>0, |Z|>1.96, H<0.5 | 0.09 |
9. 弱持续不显著减少 | S<0, |Z|<1.96, 0.5<H<0.75 | 8.27 |
10. 弱持续显著减少 | S<0, |Z|>1.96, 0.5<H<0.75 | 0.72 |
11. 强持续不显著减少 | S<0, |Z|<1.96, H>0.75 | 5.77 |
12. 强持续显著减少 | S<0, |Z|>1.96, H>0.75 | 3.97 |
Fig. 6 Correlation significance between NPP and precipitation (a), temperature (b), relative humidity (c) and sunshine hours (d) in karst areas of Yunnan, Guizhou and Guangxi
Fig. 7 The maximum response lag of NPP to the changes of precipitation (a), temperature (b), relative humidity (c) and sunshine hours (d) in the karst area of Yunnan, Guizhou and Guangxi
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