BACKGROUND Anthropogenic emissions are rapidly altering Earth's climate, pushing it
toward a warmer state for which there is no historical precedent. Although no perfect analog …

Climate tipping points occur when change in a part of the climate system becomes self-
perpetuating beyond a warming threshold, leading to substantial Earth system impacts …

Abstract We summarize historic New York City (NYC) climate change trends and provide the
latest scientific analyses on projected future changes based on a range of global …

Climate simulations: recognize the ‘hot model’ problem Skip to main content Thank you for
visiting nature.com. You are using a browser version with limited support for CSS. To obtain the …

This chapter assesses simulations of future global climate change, spanning time horizons
from the near term (2021–2040), mid-term (2041–2060), and long term (2081–2100) out to …

The future surface mass balance (SMB) will influence the ice dynamics and the contribution
of the Antarctic ice sheet (AIS) to the sea level rise. Most of recent Antarctic SMB projections …

Future climate projections show a marked increase in Greenland Ice Sheet (GrIS) runoff
during the 21st century, a direct consequence of the Polar Amplification signal. Regional …

The Holocene thermal maximum, a period of global warmth evident in early to mid-Holocene
proxy reconstructions, is controversial. Most model simulations of the Holocene have not …

In this updated and expanded edition of climate scientist Steven Koonin's groundbreaking
book, go behind the headlines to discover the latest eye-opening data about climate change …

The geological record encodes the relationship between climate and atmospheric carbon
dioxide (CO2) over long and short timescales, as well as potential drivers of evolutionary …