Changing state of the climate system
2 Chapter 2 assesses observed large-scale changes in climate system drivers, key climate
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …
[HTML][HTML] 近500 年西沙群岛海面温度年际变化的珊瑚记录及其环境意义
陶士臣， 张会领， 余克服， 施祺， 孟敏， 严宏强， 刘国辉… - 第四纪研究, 2021 - html.rhhz.net
在南海西沙群岛(15.76~ 17.13 N, 111.18~ 112.90 E) 5 条年分辨率的滨珊瑚生长率(即每年生长
宽度, mm/a 或cm/a) 序列和4 个U-Th 年龄的基础上, 根据珊瑚生长率与器测海温的显著正相关 …
宽度, mm/a 或cm/a) 序列和4 个U-Th 年龄的基础上, 根据珊瑚生长率与器测海温的显著正相关 …
Reevaluating the Little Ice Age: Novel insights from oceanic and terrestrial records on unexpected warm winters
This investigation into the Little Ice Age (LIA) climate discrepancies explores sea surface
temperature (SST) anomalies in the South China Sea (SCS) using monthly resolved coral …
temperature (SST) anomalies in the South China Sea (SCS) using monthly resolved coral …
Early onset of aridity in the past millennium: Insights from vegetation dynamics and climate change in the alpine, cold-desert region of Trans Himalaya, India
Palynological analysis of surface soil and sub-surface sediments from the outwash plain of
Hamtah Glacier, Lahaul-Spiti, India, has brought out the vegetation and climatic changes in …
Hamtah Glacier, Lahaul-Spiti, India, has brought out the vegetation and climatic changes in …
Anthropogenic effects on tropical oceanic climate change and variability: An insight from the South China Sea over the past 2000 years
To better understand the effect of human activities on tropical oceanic climate change,
existing coral-based paleoclimate data from the northern South China Sea (SCS) for several …
existing coral-based paleoclimate data from the northern South China Sea (SCS) for several …
Coral paleoclimate perspectives support the role of low‐latitude forcing on the 4.2 ka BP event
The 4.2 ka BP Event is an abrupt climate change that might have contributed to the collapse
of ancient civilizations and marks the transition between the mid‐and late‐Holocene …
of ancient civilizations and marks the transition between the mid‐and late‐Holocene …
Warming and cooling: the medieval climate anomaly in Africa and Arabia
Abstract The Medieval Climate Anomaly (MCA) is a well‐recognized climate perturbation in
many parts of the world, with a core period of 1000–1200 Common Era. Here we present a …
many parts of the world, with a core period of 1000–1200 Common Era. Here we present a …
Coral Sr/Ca-derived seasonal sea surface temperature variations in the Qiongdong upwelling area of the northern South China Sea during the Medieval Climate …
Geological records of seasonal sea surface temperature (SST) records are useful for better
understanding the past dynamics of coastal upwelling, and for inferring future scenarios. By …
understanding the past dynamics of coastal upwelling, and for inferring future scenarios. By …
South Pacific Subtropical High from the late Holocene to the end of the 21st century: insights from climate proxies and general circulation models
The South Pacific Subtropical High (SPSH) is a predominant feature of the South American
climate. The variability of this high-pressure center induces changes in the intensity of …
climate. The variability of this high-pressure center induces changes in the intensity of …
Coral‐derived western Pacific tropical sea surface temperatures during the last millennium
Reconstructions of ocean temperatures prior to the industrial era serve to constrain natural
climate variability on decadal to centennial timescales, yet relatively few such observations …
climate variability on decadal to centennial timescales, yet relatively few such observations …