STUDY ON THE TREND OF VEGETATION PHENOLOGICAL CHANGE AND ITS RESPONSE TOn   CLIMATE CHANGE IN CHANGBAI MOUNTAINS

Wang Yanying; Hou Guanglei; Zhao Jianjun; Chen Tingting; Zhang Hongyan

首页> 外文期刊>Fresenius Environmental Bulletin >STUDY ON THE TREND OF VEGETATION PHENOLOGICAL CHANGE AND ITS RESPONSE TOn CLIMATE CHANGE IN CHANGBAI MOUNTAINS

【24h】

STUDY ON THE TREND OF VEGETATION PHENOLOGICAL CHANGE AND ITS RESPONSE TOn CLIMATE CHANGE IN CHANGBAI MOUNTAINS

机译：长白山植被物候变化趋势及其对气候变化的响应研究。

获取原文

获取原文并翻译 | 示例

掌桥外文数据库（机构版） >>

开具论文收录证明 >>

文献代查 >>

页面导航

摘要
著录项
相似文献
相关主题

摘要

As one of the sensitive indicators in response to climate change, plant phonological change is usually used as an important component of dynamic vegetation models to reflect the dynamic of carbon and water exchange between the land surface and the atmosphere. The phenological change in large scale can not only reflect the seasonal variation patterns of vegetation, but also be an indicator of global climate change. In this study, using the biweekly NOAA/GIMMS NDVI (Normalized Difference Vegetatio

机译：植物物候变化作为响应气候变化的敏感指标之一，通常被用作动态植被模型的重要组成部分，以反映地表与大气之间的碳和水交换动态。物候的大范围变化不仅可以反映植被的季节变化规律，而且可以作为全球气候变化的指标。在这项研究中，使用两周一次的NOAA / GIMMS NDVI（归一化差异植被）

著录项

来源
《Fresenius Environmental Bulletin》 |2015年第6a期|2193-2202|共10页
作者
Wang Yanying; Hou Guanglei; Zhao Jianjun; Chen Tingting; Zhang Hongyan;
展开▼
作者单位

NE Normal Univ, Sch Geog Sci, Changchun, Jilin Province, Peoples R China.;

Chinese Acad Sci, Northeast Inst Geog & Agroecol, Changchun, Peoples R China.;

NE Normal Univ, Sch Geog Sci, Changchun, Jilin Province, Peoples R China.;

Hong Kong Polytech Univ, Dept Bldg & Real Estate, Hong Kong, Hong Kong, Peoples R China.;

NE Normal Univ, Sch Geog Sci, Changchun, Jilin Province, Peoples R China.;

展开▼
收录信息
原文格式 PDF
正文语种 eng
中图分类
关键词
Changbai Mountains; Climate zones; GIMMS NDVI; Onset date of green-up; Onset date of dormancy;

机译：长白山;气候带;GIMMS NDVI;绿化的开始日期;休眠的开始日期;

相似文献

外文文献
中文文献
专利

1. STUDY ON THE TREND OF VEGETATION PHENOLOGICAL CHANGE AND ITS RESPONSE TO CLIMATE CHANGE IN CHANGBAI MOUNTAINS [J] . Yanying Wang, Guanglei Hou, Hongyan Zhang, Fresenius environmental bulletin . 2015,第6A期

机译：长白山植被物候变化趋势及其对气候变化的响应研究
2. Forest vegetation responses to climate and environmental change: a case study from Changbai Mountain, NE China. [J] . Bai Fan, Sang WeiGuo, Axmacher J. C. Forest Ecology and Management . 2011,第11期

机译：森林植被对气候和环境变化的响应：以中国东北长白山为例。
3. Vegetation Phenological Changes in Multiple Landforms and Responses to Climate Change [J] . Progress in Artificial Intelligence . 2020,第2期

机译：多种地貌的植被鉴定和气候变化的反应
4. Vegetation change during 1990-2000 and its response to climate change in the northern slope of Tianshan Mountains [C] . Geping Luo, Xi Chen Geoscience and Remote Sensing Symposium, 2004. IGARSS '04. Proceedings. 2004 IEEE International . 2004

机译：1990-2000年天山北坡植被变化及其对气候变化的响应
5. Modeling the phenological response to climate change and its impact on carbon cycle in northeastern U.S. forests [D] . Xu, Hong 2015

机译：模拟美国东北部森林对气候变化的物候响应及其对碳循环的影响
6. Trends in Global Vegetation Activity and Climatic Drivers Indicate a Decoupled Response to Climate Change [O] . Antonius G. T. Schut, Eva Ivits, Jacob G. Conijn, -1

机译：全球植被活动和气候驱动因素的趋势表明对气候变化的反应是脱钩的
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。

STUDY ON THE TREND OF VEGETATION PHENOLOGICAL CHANGE AND ITS RESPONSE TOn CLIMATE CHANGE IN CHANGBAI MOUNTAINS

摘要

著录项

相似文献

相关主题

期刊订阅