Spinous-Process
发表于 2025-3-28 18:07:13
http://reply.papertrans.cn/39/3861/386092/386092_41.png
eulogize
发表于 2025-3-28 19:33:33
https://doi.org/10.1007/978-3-8349-8407-4of processes across both steep environmental gradients and different time scales, we may be able to better estimate ecosystem responses to current and future environmental change (Ammann et al. 1993; Lotter et al. 1997).
休战
发表于 2025-3-29 01:56:16
http://reply.papertrans.cn/39/3861/386092/386092_43.png
无孔
发表于 2025-3-29 06:46:21
A Dynamical Perspective on High Altitude Paleoclimate Proxy Timeseriesevant to the study of past climatic changes (Alverson and Kull 2002). Properties recorded in these archives offer quantitative climate-related information at annual or higher temporal resolution. In addition, by nature of their occurrence at high elevation, they provide information about climate var
B-cell
发表于 2025-3-29 09:23:34
Understanding the Spatial Heterogeneity of Global Environmental Change in Mountain Regionsphysiographic complexity of mountains creates environments that can be highly variable over relatively short distances. This spatial heterogeneity reflects a hierarchy of environmental controls. At regional scales, insolation and atmospheric circulation features determine the dominant regional clima
容易懂得
发表于 2025-3-29 13:41:30
Ice Cores from Tropical Mountain Glaciers as Archives of Climate Change, and by which we will become increasingly more affected in the coming centuries. One-half of the Earth’s surface area lies in the tropics between 30°N and 30°S, and this area supports almost 70% of the global population. Thus, temporal and spatial variations in the occurrence and intensity of coupl
Encapsulate
发表于 2025-3-29 17:03:45
http://reply.papertrans.cn/39/3861/386092/386092_47.png
wangle
发表于 2025-3-29 20:58:11
http://reply.papertrans.cn/39/3861/386092/386092_48.png
破译密码
发表于 2025-3-30 03:24:54
http://reply.papertrans.cn/39/3861/386092/386092_49.png
deadlock
发表于 2025-3-30 07:05:25
Glacier-Climate Models as Palaeoclimatic Information Sources: Examples from the Alpine Younger Dryasn patterns. This is particularly true when precipitation is primarily caused by the advection of air masses to the Alps from the North Atlantic or the Mediterranean Sea, as is the case under cold conditions. Alpine precipitation patterns during the Lateglacial period can hence be interpreted in term