Publication

Climate change and Arctic ecosystems: 1. Vegetation changes north of 55 degrees N between the last glacial maximum, mid-Holocene, and present

About
Privacy
Disclaimer

Graph Chatbot

Chat with Graph Search

Ask any question about EPFL courses, lectures, exercises, research, news, etc. or try the example questions below.

DISCLAIMER: The Graph Chatbot is not programmed to provide explicit or categorical answers to your questions. Rather, it transforms your questions into API requests that are distributed across the various IT services officially administered by EPFL. Its purpose is solely to collect and recommend relevant references to content that you can explore to help you answer your questions.

Climate change and Arctic ecosystems: 1. Vegetation changes north of 55 degrees N between the last glacial maximum, mid-Holocene, and present

Graph Chatbot

Chat with Graph Search

Soil warming alters tree water use and canopy stomatal conductance in a mixed subtropical forest

Regional uniqueness of tree species composition and response to forest loss and climate change

Invasive palms have more efficient and prolonged CO2 assimilation compared to native sub-Mediterranean vegetation

From roots to canopy: Unraveling the influence of species diversity on tree water relations under warmer and drier climates

Impact of intercepted and sub-canopy snow microstructure on snowpack response to rain-on-snow events under a boreal canopy

Characteristics and sources of fluorescent aerosols in the central Arctic Ocean

Waterborne Virus Transport and Risk Assessment in Lake Geneva Under Climate Change

Flood, farms and credit: The role of branch banking in the era of climate change

Renaturation of urban rivers as a climate adaptation strategy Case study in Geneva, Switzerland

Multi-temporal forest monitoring in the Swiss Alps with knowledge-guided deep learning