Here, we review information on how plants face redox imbalance caused by climate change,
and focus on the role of nitric oxide (NO) in this response. Life on Earth is possible thanks to …

Recent progress is reviewed in the understanding of convective interaction with water vapor
and changes associated with water vapor in warmer climates. Progress includes new …

A comprehensive assessment of twenty-first century climate change in the European Alps is
presented. The analysis is based on the EURO-CORDEX regional climate model ensemble …

There is a direct influence of global warming on precipitation. Increased heating leads to
greater evaporation and thus surface drying, thereby increasing the intensity and duration of …

Global‐scale changes in water vapor and responses to surface temperature variability since
1979 are evaluated across a range of satellite and ground‐based observations, a reanalysis …

Climate models suggest that extreme precipitation events will become more common in an
anthropogenically warmed climate. However, observational limitations have hindered a …

This chapter assesses the capacity of the global climate models used elsewhere in this
report for projecting future climate change. Confidence in model estimates of future climate …

This study examines the response of the tropical atmospheric and oceanic circulation to
increasing greenhouse gases using a coordinated set of twenty-first-century climate model …

Observations and simulations link anthropogenic greenhouse and aerosol emissions with
rapidly increasing Indian Ocean sea surface temperatures (SSTs). Over the past 60 years …

In this study, using 104 years (1901–2004) of high resolution daily gridded rainfall data,
variability and long‐term trends of extreme rainfall events over central India have been …