
Regulation factors driving vegetation changes in China during the past 20 years
ZHAO Haixia, GU Binjie, LINDLEY Sarah, ZHU Tianyuan, FAN Jinding
Journal of Geographical Sciences ›› 2023, Vol. 33 ›› Issue (3) : 508-528.
Regulation factors driving vegetation changes in China during the past 20 years
Vegetation change is of significant concern because it plays a crucial role in the global carbon cycle and climate. Many studies have examined recent changes in vegetation growth and the associated drivers. These drivers include both natural and human activities, but few studies have identified the regulation factors. By employing normalized difference vegetation index (NDVI) data, we analyzed the spatiotemporal pattern of vegetation change in China and then explored the driving factors. It was found that the overall greening of China has improved significantly, especially in the Loess Plateau and southwest China. The Yangtze River Delta and Bohai Rim, however, have not seen as much growth. Natural conditions are conducive to vegetation growth. Although socioeconomic development will be more beneficial for vegetation restoration, the current level and speed of development have a negative effect on vegetation. The regulation factors are considered separately since they affect both directly and indirectly. Regulation factors have accelerated vegetation growth. By understanding the factors affecting the current vegetation growth, we can provide a guide for future vegetation recovery in China and other similar countries.
vegetation change / NDVI / regulation factors / climate change / China {{custom_keyword}} /
Table 1 The dependent and independent variables |
Variables | Instructions |
---|---|
Tem | Average air temperature in provincial regions (℃) |
Pre | Average precipitation in provincial regions (mm) |
GDPpc | Per capita GDP (yuan per person) |
Land-use | Construction land area/Total area (%) |
Rural | The number of rural residents (10 thousand people) |
Carbon | Annual carbon emissions in provincial regions (Mt CO2) |
Investment | Investment in agricultural and forestry fixed assets in provincial regions (100 million yuan) |
Policy&Law | The annual number of policies and regulations issued by provincial regions |
DummyVar | Set it to 0 before 2018 and 1 after 2018 |
NDVI | The dependent variable |
Table 2 Classification of vegetation cover in 2000, 2010 and 2019 |
Levels | 2000 | 2010 | 2019 | |||
---|---|---|---|---|---|---|
Area (km2) | Proportion (%) | Area (km2) | Proportion (%) | Area (km2) | Proportion (%) | |
Low | 2656560 | 28.09 | 2391200 | 25.28 | 2455382 | 25.96 |
Medium-low | 1073466 | 11.35 | 1056010 | 11.17 | 968517 | 10.24 |
Medium | 1044075 | 11.04 | 910148 | 9.62 | 845327 | 8.94 |
Medium-high | 3841472 | 40.62 | 2689320 | 28.43 | 1862571 | 19.69 |
High | 842643 | 8.91 | 2411538 | 25.50 | 3326419 | 35.17 |
Table 3 NDVI and the slope of NDVI in different provincial-level regions of China in 2000, 2010 and 2019 |
Provincial-level region | 2000 | 2005 | 2010 | 2015 | 2019 | Slope |
---|---|---|---|---|---|---|
Shanghai | 0.5774 | 0.5257 | 0.5084 | 0.5034 | 0.5081 | -0.00342 |
Jiangsu | 0.7038 | 0.7279 | 0.7452 | 0.6810 | 0.6902 | -0.00152 |
Tianjin | 0.6160 | 0.6624 | 0.6673 | 0.6102 | 0.6420 | -0.00001 |
Shandong | 0.6911 | 0.7345 | 0.7042 | 0.6999 | 0.7102 | 0.00007 |
Xinjiang | 0.1744 | 0.1879 | 0.2194 | 0.1764 | 0.1855 | 0.00025 |
Qinghai | 0.3400 | 0.3614 | 0.3855 | 0.3583 | 0.3773 | 0.00149 |
Xizang | 0.2866 | 0.3089 | 0.2998 | 0.3095 | 0.3238 | 0.00155 |
Taiwan | 0.7674 | 0.7952 | 0.7892 | 0.7971 | 0.8036 | 0.00155 |
Zhejiang | 0.7480 | 0.7634 | 0.7835 | 0.7775 | 0.7782 | 0.00158 |
Anhui | 0.7351 | 0.7935 | 0.8147 | 0.7789 | 0.7884 | 0.00196 |
Henan | 0.7311 | 0.7728 | 0.7906 | 0.7742 | 0.7823 | 0.00219 |
Beijing | 0.6977 | 0.7225 | 0.7168 | 0.7385 | 0.7448 | 0.00230 |
Inner Mongolia | 0.4127 | 0.4528 | 0.4468 | 0.4539 | 0.4753 | 0.00262 |
Hubei | 0.7362 | 0.7808 | 0.8000 | 0.8037 | 0.8041 | 0.00335 |
Jiangxi | 0.7285 | 0.7628 | 0.7775 | 0.7982 | 0.7948 | 0.00354 |
Hebei | 0.6739 | 0.7311 | 0.7433 | 0.7319 | 0.7587 | 0.00356 |
Chongqing | 0.7532 | 0.7752 | 0.7905 | 0.8152 | 0.8254 | 0.00385 |
Hunan | 0.7331 | 0.7673 | 0.7827 | 0.8055 | 0.8079 | 0.00394 |
Heilongjiang | 0.7780 | 0.8433 | 0.8457 | 0.8658 | 0.8612 | 0.00400 |
Guangdong | 0.7014 | 0.7370 | 0.7439 | 0.7694 | 0.7829 | 0.00408 |
Fujian | 0.7440 | 0.7802 | 0.7825 | 0.8197 | 0.8252 | 0.00422 |
Liaoning | 0.7128 | 0.7860 | 0.8050 | 0.7955 | 0.8084 | 0.00423 |
Hainan | 0.7455 | 0.7663 | 0.7917 | 0.8220 | 0.8222 | 0.00439 |
Gansu | 0.3375 | 0.3705 | 0.3865 | 0.3987 | 0.4369 | 0.00470 |
Sichuan | 0.6935 | 0.7313 | 0.7327 | 0.7781 | 0.7836 | 0.00475 |
Jilin | 0.7408 | 0.8022 | 0.8200 | 0.8333 | 0.8394 | 0.00481 |
Guangxi | 0.7263 | 0.7656 | 0.7877 | 0.8196 | 0.8318 | 0.00554 |
Guizhou | 0.7188 | 0.7548 | 0.7815 | 0.8246 | 0.8252 | 0.00593 |
Yunnan | 0.7046 | 0.7570 | 0.7562 | 0.8136 | 0.8319 | 0.00648 |
Shanxi | 0.5919 | 0.6298 | 0.6715 | 0.6903 | 0.7194 | 0.00658 |
Shaanxi | 0.5991 | 0.6603 | 0.6939 | 0.7176 | 0.7426 | 0.00720 |
Ningxia | 0.2914 | 0.3124 | 0.3973 | 0.3842 | 0.4613 | 0.00852 |
Figure 5 Results of multiple regression analysisNote: The model’s R is 0.710, which reflects a high degree of linear correlation between all the independent variables and NDVI. The R2 is 0.505, which indicates that 50.5% of the NDVI could be explained by all the independent variables. Sig. in the model is 1.039×10-9, which is less than 0.05. It proves that the variables are correlated. |
Table 4 The target and implementation of forest cover rate from 10th to 14th Five-Year Plan periods |
Five-Year Plan for China’s National Economic and Social Development | 10th | 11th | 12th | 13th | 14th |
---|---|---|---|---|---|
The target of forest cover rate (%) | 18.20 | 20.0 | 21.66 | 23.04 | 24.10 |
The implementation of forest cover rate (%) | 18.20 | 20.36 | 21.66 | 23.20 | / |
Notes: The 10th Five-Year Plan runs from 2000 to 2005, and so on to the 14th Five-Year Plan from 2020 to 2025. The implementation of forest cover rate is in 2005, 2010, 2015 and 2019 respectively, but it is temporarily blank because the target year of the 14th Five-Year Plan is 2025. |
Table 5 Chinese laws and regulations on vegetation protection and growth |
Laws | Regulations | |
---|---|---|
The national level | The provincial level | |
Forest Law of the People’s Republic of China (2019 Revision) | Regulations of the People’s Republic of China on Nature Reserves (2017 Revision) | Regulations of Guizhou Province on the Administration of Forest Land (2018 Revision) |
Grassland Law of the People’s Republic of China (2013 Revision) | Regulations on the Administration of Construction Project Protection (2017 Revision) | Regulations of Shaanxi Province on Forest Management (2000 Revision) |
Environmental Protection Law of People’s Republic of China (2014 Revision) | Management Rules of Felling and Regeneration of Forest (2011 Revision) | Measures of Yunnan Province for the Administration of Nature Reserves (2018 Revision) |
Air Pollution Prevention Law of the People’s Republic of China (2015 Revision) | Environmental Protection Rule of Guangdong province (2018 Revision) | |
Agriculture Law of the People’s Republic of China (2012 Revision) | Regulations of Jilin Province on ecological environment Protection (2020 Revision) | |
Prevention and Control of Desertification Law of the People’s Republic of China (2018 Revision) | Measures of Heilongjiang Province for Residential Environment Protection (2018 Revision) | |
Water and Soil Conservation Law of the People’s Republic of China (2010 Revision) | Measures of Hebei Province for the Administration of Environmental Monitoring (2013 Revision) | |
The Environmental Effect Evaluation Legislation of the People’s Republic of China (2018 Revision) | …… |
Notes: Provincial regulations are incomplete statistics and some representative regulations are selected. |
[1] |
Climate change extreme events have consequential impacts that influence the responses of vegetation dynamics as well as ecosystem functioning and sustainable human well-being. Therefore, vegetation response to climate change (VRCC) needs to be explored to foster specific-organised management programmes towards ecological conservation and targeted restoration policy to various climate extreme threats. This review aimed to explore the existing literature to characterise VRCC and to identify solutions and techniques fundamental in designing strategies for targeted effective adaptation and mitigation to achieve sustainable planning outcomes. Accordingly, this review emphasised recent theoretical and practical research on the vegetation-climate responses and their related impacts in the wake of climate change and its debilitating impacts on vegetation. Consequently, this study proposes the Information-based model (IBM), needed to examine Factors–forms of Impacts–Solutions (Techniques)–Risks assessment to identify and provide insights about VRCC in a given region. In conclusion, two enablers of adaptive indicators and the novel systems-based serve as a key policy formulation for sustainability in strengthening the goals of global involvement of local and sub-national governments and institutions in the effective management of vegetation and ecosystem protection.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[2] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[3] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[4] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[5] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[6] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[7] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[8] |
Satellite data show increasing leaf area of vegetation due to direct (human land-use management) and indirect factors (climate change, CO fertilization, nitrogen deposition, recovery from natural disturbances, etc.). Among these, climate change and CO fertilization effect seem to be the dominant drivers. However, recent satellite data (2000-2017) reveal a greening pattern that is strikingly prominent in China and India, and overlapping with croplands world-wide. China alone accounts for 25% of the global net increase in leaf area with only 6.6% of global vegetated area. The greening in China is from forests (42%) and croplands (32%), but in India is mostly from croplands (82%) with minor contribution from forests (4.4%). China is engineering ambitious programs to conserve and expand forests with the goal of mitigating land degradation, air pollution and climate change. Food production in China and India has increased by over 35% since 2000 mostly due to increasing harvested area through multiple cropping facilitated by fertilizer use and surface/ground-water irrigation. Our results indicate that the direct factor is a key driver of the "Greening Earth", accounting for over a third, and likely more, of the observed net increase in green leaf area. They highlight the need for realistic representation of human land-use practices in Earth system models.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[9] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[10] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[11] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[12] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[13] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[14] |
Contents Summary 652 I. Introduction 652 II. Discrepancy in predicting the effects of rising [CO ] on the terrestrial C sink 655 III. Carbon and nutrient storage in plants and its modelling 656 IV. Modelling the source and the sink: a plant perspective 657 V. Plant-scale water and Carbon flux models 660 VI. Challenges for the future 662 Acknowledgements 663 Authors contributions 663 References 663 SUMMARY: The increase in atmospheric CO in the future is one of the most certain projections in environmental sciences. Understanding whether vegetation carbon assimilation, growth, and changes in vegetation carbon stocks are affected by higher atmospheric CO and translating this understanding in mechanistic vegetation models is of utmost importance. This is highlighted by inconsistencies between global-scale studies that attribute terrestrial carbon sinks to CO stimulation of gross and net primary production on the one hand, and forest inventories, tree-scale studies, and plant physiological evidence showing a much less pronounced CO fertilization effect on the other hand. Here, we review how plant carbon sources and sinks are currently described in terrestrial biosphere models. We highlight an uneven representation of complexity between the modelling of photosynthesis and other processes, such as plant respiration, direct carbon sinks, and carbon allocation, largely driven by available observations. Despite a general lack of data on carbon sink dynamics to drive model improvements, ways forward toward a mechanistic representation of plant carbon sinks are discussed, leveraging on results obtained from plant-scale models and on observations geared toward model developments.© 2018 The Authors. New Phytologist © 2018 New Phytologist Trust.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[15] |
Vegetation cover plays a key role in terrestrial ecosystem; therefore, it is important for researchers to investigate the variation and influencing factors of vegetation cover. China has experienced a large-scale vegetation cover change in recent years. We summarized the literature of vegetation cover change and revealed how large-scale anthropogenic activities influence vegetation cover change in China. Afforestation and intensification of cropland played a key role in large-scale greening. Urbanization showed a “U” shape to influence vegetation cover change. Mining and reclamation, land abandonment and land consolidation, and regional natural protection all had a unique influence on the change of vegetation cover. Indeed, the large-scale vegetation cover change was caused by interaction of anthropogenic factors and part human-driven climate change. Anthropogenic factors influenced climate change to indirectly alter the condition of plant growth. Interaction between climate change and human activities influence on vegetation cover still needs to be further investigated in the future.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[16] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[17] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[18] |
A large body of literature is available on wound healing in humans. Nonetheless, a standardized ex vivo wound model without disruption of the dermal compartment has not been put forward with compelling justification. Here, we present a novel wound model based on application of negative pressure and its effects for epidermal regeneration and immune cell behaviour. Importantly, the basement membrane remained intact after blister roof removal and keratinocytes were absent in the wounded area. Upon six days of culture, the wound was covered with one to three-cell thick K14+Ki67+ keratinocyte layers, indicating that proliferation and migration were involved in wound closure. After eight to twelve days, a multi-layered epidermis was formed expressing epidermal differentiation markers (K10, filaggrin, DSG-1, CDSN). Investigations about immune cell-specific manners revealed more T cells in the blister roof epidermis compared to normal epidermis. We identified several cell populations in blister roof epidermis and suction blister fluid that are absent in normal epidermis which correlated with their decrease in the dermis, indicating a dermal efflux upon negative pressure. Together, our model recapitulates the main features of epithelial wound regeneration, and can be applied for testing wound healing therapies and investigating underlying mechanisms.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[19] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[20] |
Though many studies have focused on the causes of shifts in trend of temperature, whether the response of vegetation growth to temperature has changed is still not very clear. In this study, we analyzed the spatial features of the trend changes of temperature during the growing season and the response of vegetation growth in China based on observed climatic data and the normalized difference vegetation index (NDVI) from 1984 to 2011. An obvious warming to cooling shift during growing season from the period 1984-1997 to the period 1998-2011 was identified in the northern and northeastern regions of China, whereas a totally converse shift was observed in the southern and western regions, suggesting large spatial heterogeneity of changes of the trend of growing season temperature throughout China. China as a whole, a significant positive relationship between vegetation growth and temperature during 1984 to 1997 has been greatly weakened during 1998-2011. This change of response of vegetation growth to temperature has also been confirmed by Granger causality test. On regional scales, obvious shifts in relationship between vegetation growth and temperature were identified in temperate desert region and rainforest region. Furthermore, by comprehensively analyzing of the relationship between NDVI and climate variables, an overall reduction of impacts of climate factors on vegetation growth was identified over China during recent years, indicating enhanced influences from human associated activities. {{custom_citation.content}}
{{custom_citation.annotation}}
|
[21] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[22] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[23] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[24] |
Since the 1970s, installed solar photovoltaic capacity has grown tremendously to 230 gigawatt worldwide in 2015, with a growth rate between 1975 and 2015 of 45%. This rapid growth has led to concerns regarding the energy consumption and greenhouse gas emissions of photovoltaics production. We present a review of 40 years of photovoltaics development, analysing the development of energy demand and greenhouse gas emissions associated with photovoltaics production. Here we show strong downward trends of environmental impact of photovoltaics production, following the experience curve law. For every doubling of installed photovoltaic capacity, energy use decreases by 13 and 12% and greenhouse gas footprints by 17 and 24%, for poly- and monocrystalline based photovoltaic systems, respectively. As a result, we show a break-even between the cumulative disadvantages and benefits of photovoltaics, for both energy use and greenhouse gas emissions, occurs between 1997 and 2018, depending on photovoltaic performance and model uncertainties.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[25] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[26] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[27] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[28] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[29] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[30] |
Climate-driven vegetation mortality is occurring globally and is predicted to increase in the near future. The expected climate feedbacks of regional-scale mortality events have intensified the need to improve the simple mortality algorithms used for future predictions, but uncertainty regarding mortality processes precludes mechanistic modeling. By integrating new evidence from a wide range of fields, we conclude that hydraulic function and carbohydrate and defense metabolism have numerous potential failure points, and that these processes are strongly interdependent, both with each other and with destructive pathogen and insect populations. Crucially, most of these mechanisms and their interdependencies are likely to become amplified under a warmer, drier climate. Here, we outline the observations and experiments needed to test this interdependence and to improve simulations of this emergent global phenomenon.Copyright © 2011 Elsevier Ltd. All rights reserved.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[31] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[32] |
It is confirmed that China has been greening over the last two decades. Such greening and its driving factors are therefore significant for understanding the relationship between vegetation and environments. However, studies on vegetation changes and attribution analyses at the national scale are limited in China after 2000. In this study, fractional vegetation cover (FVC) data from Global Land Surface Satellite (GLASS) was used to detect vegetation change trends from 2001 to 2018, and the effects of CO2, temperature, shortwave radiation, precipitation, and land cover change (LCC) on FVC changes were quantified using generalized linear models (GLM). The results showed that (1) FVC in China increased by 14% from 2001 to 2018 with a greening rate of approximately 0.0019/year (p < 0.01), which showed an apparent greening trend. (2) On the whole, CO2, climate-related factors, and LCC accounted for 88% of FVC changes in China, and the drivers explained 82%, 89%, 90%, and 89% of the FVC changes in the Qinghai–Tibet region, northwest region, northern region, and southern region, respectively. CO2 was the major driving factor for FVC changes, accounting for 31% of FVC changes in China, indicating that CO2 was an essential factor in vegetation growth research. (3) The statistical results of pixels with land cover changes showed that LCC explained 12% of FVC changes, LCC has played a relatively important role and this phenomenon may be related to the ecological restoration projects. This study enriches the study of vegetation changes and its driving factors, and quantitatively describes the response relationship between vegetation and its driving factors. The results have an important significance for adjusting terrestrial ecosystem services.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[33] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[34] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[35] |
Using satellite-derived normalized difference vegetation index (NDVI) data, several previous studies have indicated that vegetation growth significantly increased in most areas of China during the period 1982–99. In this letter, we extended the study period to 2010. We found that at the national scale the growing season (April–October) NDVI significantly increased by 0.0007 yr−1 from 1982 to 2010, but the increasing trend in NDVI over the last decade decreased in comparison to that of the 1982–99 period. The trends in NDVI show significant seasonal and spatial variances. The increasing trend in April and May (AM) NDVI (0.0013 yr−1) is larger than those in June, July and August (JJA) (0.0003 yr−1) and September and October (SO) (0.0008 yr−1). This relatively small increasing trend of JJA NDVI during 1982–2010 compared with that during 1982–99 (0.0012 yr−1) (Piao et al 2003 J. Geophys. Res.—Atmos. \n 108 4401) implies a change in the JJA vegetation growth trend, which significantly turned from increasing (0.0039 yr−1) to slightly decreasing ( − 0.0002 yr−1) in 1988. Regarding the spatial pattern of changes in NDVI, the growing season NDVI increased (over 0.0020 yr−1) from 1982 to 2010 in southern China, while its change was close to zero in northern China, as a result of a significant changing trend reversal that occurred in the 1990s and early 2000s. In northern China, the growing season NDVI significantly increased before the 1990s as a result of warming and enhanced precipitation, but decreased after the 1990s due to drought stress strengthened by warming and reduced precipitation. Our results also show that the responses of vegetation growth to climate change vary across different seasons and ecosystems.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[36] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[37] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[38] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[39] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[40] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[41] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[42] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[43] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[44] |
Despite China’s emissions having plateaued in 2013, it is still the world’s leading energy consumer and CO2 emitter, accounting for approximately 30% of global emissions. Detailed CO2 emission inventories by energy and sector have great significance to China’s carbon policies as well as to achieving global climate change mitigation targets. This study constructs the most up-to-date CO2 emission inventories for China and its 30 provinces, as well as their energy inventories for the years 2016 and 2017. The newly compiled inventories provide key updates and supplements to our previous emission dataset for 1997–2015. Emissions are calculated based on IPCC (Intergovernmental Panel on Climate Change) administrative territorial scope that covers all anthropogenic emissions generated within an administrative boundary due to energy consumption (i.e. energy-related emissions from 17 fossil fuel types) and industrial production (i.e. process-related emissions from cement production). The inventories are constructed for 47 economic sectors consistent with the national economic accounting system. The data can be used as inputs to climate and integrated assessment models and for analysis of emission patterns of China and its regions.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[45] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[46] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[47] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[48] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[49] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[50] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[51] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[52] |
The extent to which an urbanization effect has contributed to climate warming is under debate in China. Some previous studies have shown that the urban heat island (UHI) contribution to national warming was substantial (10%–40%). However, by considering the spatial scale of urbanization effects, this study indicates that the UHI contribution is negligible (less than 1%). Urban areas constitute only 0.7% of the whole of China. According to the proportions of urban and rural areas used in this study, the weighted urban and rural temperature averages reduced the estimated total warming trend and also reduced the estimated urban effects. Conversely, if all stations were arithmetically averaged, that is, without weighting, the total warming trend and urban effects will be overestimated as in previous studies because there are more urban stations than rural stations in China. Moreover, the urban station proportion (68%) is much higher than the urban area proportion (0.7%).
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[53] |
Based on MODIS-NDVI and climate data, using an artificial influence model based on coefficient of variation to quantitatively calculate the human impact of vegetation cover(NDVIH) in China from 2001 to 2015, Sen+Mann-Kendall model and Hurst index were used to analyze the spatial-temporal feature and the future trends. It was found that: (1) In the year from 2001 to 2015, the Spatial Differentiation of NDVIH in China was more obvious from southern part to northern part, with an average annual mean value of -0.0102, the vegetation coverage decreased slightly under human activities, the negative impact area accounting for 51.59% which is slightly larger than the positive impact area. (2) The interannual variation of NDVIH in China is obvious, showing the negative impact volatility decreased, the rate of decline is 0.5%/10a; among which the positive and negative effects all showed an increasing trend, the positive growth rate (0.3%/10a) is much larger than the negative impact (0.02%/10a). (3) During 2001-2015, the center of gravity of positive impact has moved to the northeast, the center of gravity of negative impact has moved to the southwest, vegetation cover in northeastern China has improved under the influence of mankind, and human activities in the southwest have increased the degree of vegetation destruction. (4) The proportion of "negative impact reduction" and "positive impact increase" trend of NDVIH in China appeared to be the largest which accounting for 28.14% and 25.21% of the total, and the ecological environment is improving. (5) The reverse characteristics of NDVIH change were stronger than the same characteristic in China, mainly showed a negative impact which decreased at the first and then increased with the rate of 15.59% of the total area. {{custom_citation.content}}
{{custom_citation.annotation}}
|
[54] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[55] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[56] |
Global climate change has led to significant changes in seasonal rhythm events of vegetation growth, such as spring onset and autumn senescence. Spatiotemporal shifts in these vegetation phenological metrics have been widely reported over the globe. Vegetation growth peak represents plant photosynthesis capacity and responds to climate change. At present, spatiotemporal changes in vegetation growth peak characteristics (timing and maximum growth magnitude) and their underlying governing mechanisms remain unclear at regional scales. In this study, the spatiotemporal dynamics of vegetation growth peak in northeast China (NEC) was investigated using long-term NDVI time series. Then, the effects of climatic factors and spring phenology on vegetation growth peak were examined. Finally, the contribution of growth peak to vegetation production variability was estimated. The results of the phenological analysis indicate that the date of vegetation green up in spring and growth peak in summer generally present a delayed trend, while the amplitude of growth peak shows an increasing trend. There is an underlying cycle of 11 years in the vegetation growth peak of the entire study area. Air temperature and precipitation before the growing season have a small impact on vegetation growth peak amplitude both in its spatial extent and magnitude (mainly over grasslands) but have a significant influence on the date of the growth peak in the forests of the northern area. Spring green-up onset has a more significant impact on growth peak than air temperature and precipitation. Although green-up date plays a more pronounced role in controlling the amplitude of the growth peak in forests and grasslands, it also affects the date of growth peak in croplands. The amplitude of the growth peak has a significant effect on the inter-annual variability of vegetation production. The discrepant patterns of growth peak response to climate and phenology reflect the distinct adaptability of the vegetation growth peak to climate change, and result in different carbon sink patterns over the study area. The study of growth peak could improve our understanding of vegetation photosynthesis activity over various land covers and its contribution to carbon uptake.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[57] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[58] |
Climate conditions significantly affect vegetation growth in terrestrial ecosystems. Due to the spatial heterogeneity of ecosystems, the vegetation responses to climate vary considerably with the diverse spatial patterns and the time-lag effects, which are the most important mechanism of climate-vegetation interactive effects. Extensive studies focused on large-scale vegetation-climate interactions use the simultaneous meteorological and vegetation indicators to develop models; however, the time-lag effects are less considered, which tends to increase uncertainty. In this study, we aim to quantitatively determine the time-lag effects of global vegetation responses to different climatic factors using the GIMMS3g NDVI time series and the CRU temperature, precipitation, and solar radiation datasets. First, this study analyzed the time-lag effects of global vegetation responses to different climatic factors. Then, a multiple linear regression model and partial correlation model were established to statistically analyze the roles of different climatic factors on vegetation responses, from which the primary climate-driving factors for different vegetation types were determined. The results showed that (i) both the time-lag effects of the vegetation responses and the major climate-driving factors that significantly affect vegetation growth varied significantly at the global scale, which was related to the diverse vegetation and climate characteristics; (ii) regarding the time-lag effects, the climatic factors explained 64% variation of the global vegetation growth, which was 11% relatively higher than the model ignoring the time-lag effects; (iii) for the area with a significant change trend (for the period 1982-2008) in the global GIMMS3g NDVI (P < 0.05), the primary driving factor was temperature; and (iv) at the regional scale, the variation in vegetation growth was also related to human activities and natural disturbances. Considering the time-lag effects is quite important for better predicting and evaluating the vegetation dynamics under the background of global climate change. © 2015 John Wiley & Sons Ltd.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[59] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[60] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[61] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[62] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[63] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[64] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
[65] |
Global environmental change is rapidly altering the dynamics of terrestrial vegetation, with consequences for the functioning of the Earth system and provision of ecosystem services(1,2). Yet how global vegetation is responding to the changing environment is not well established. Here we use three long-term satellite leaf area index (LAI) records and ten global ecosystem models to investigate four key drivers of LAI trends during 1982-2009. We show a persistent and widespread increase of growing season integrated LAI (greening) over 25% to 50% of the global vegetated area, whereas less than 4% of the globe shows decreasing LAI (browning). Factorial simulations with multiple global ecosystem models suggest that CO2 fertilization effects explain 70% of the observed greening trend, followed by nitrogen deposition (9%), climate change (8%) and land cover change (LCC) (4%). CO2 fertilization effects explain most of the greening trends in the tropics, whereas climate change resulted in greening of the high latitudes and the Tibetan Plateau. LCC contributed most to the regional greening observed in southeast China and the eastern United States. The regional effects of unexplained factors suggest that the next generation of ecosystem models will need to explore the impacts of forest demography, differences in regional management intensities for cropland and pastures, and other emerging productivity constraints such as phosphorus availability.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
{{custom_ref.label}} |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
/
〈 |
|
〉 |