Warming amplification over the Arctic Pole (AP hereafter) and Third Pole (Tibetan Plateau,
TP hereafter) can trigger a series of climate responses and have global consequences …

Abstract The Tibetan Plateau (TP) is also known as the “Third Pole”. Elevation dependent
warming (EDW), the phenomenon that warming rate changes systematically with elevation …

This chapter assesses the causes of observed changes assessed in Chapters 2 to 5 and
uses understanding of physical processes, climate models and statistical approaches. The …

Climate models have become the most powerful tool not only for predicting climate change
but also for understanding it. Here, I discuss the role of greenhouse gases such as carbon …

Despite continued growth in atmospheric levels of greenhouse gases, global mean surface
and tropospheric temperatures have shown slower warming since 1998 than previously …

Observed Temperature Changes in the Troposphere and Stratosphere from 1979 to 2018 in:
Journal of Climate Volume 33 Issue 19 (2020) Jump to Content Jump to Main Navigation …

Ozone changes and associated climate impacts in the Coupled Model Intercomparison
Project Phase 5 (CMIP5) simulations are analyzed over the historical (1960–2005) and …

In 1967, scientists used a simple climate model to predict that human-caused increases in
atmospheric CO2 should warm Earth's troposphere and cool the stratosphere. This …

How much can we trust model-based projections of future anthropogenic climate change?
This review attempts to give an overview of this important but difficult topic by using three …

An updated analysis of observed stratospheric temperature variability and trends is
presented on the basis of satellite, radiosonde, and lidar observations. Satellite data include …