China is facing hotter and longer heat waves and more frequent and unpredictable heavy rain as a result of climate change, the weather bureau warned, as the world's second-biggest economy braces for another scorching summer.

In its annual climate "Blue Book", the China Meteorological Administration (CMA) warned that maximum temperatures across the country could rise by 1.7-2.8 degrees Celsius within 30 years, with eastern China and the northwestern region of Xinjiang set to suffer the most.

Last year, average national temperatures hit a new high, leading to record levels of glacial retreat and melting permafrost in the northwest, the Blue Book said.

China describes itself as one of the world's most climate-vulnerable countries, and it is coming under increasing pressure to adapt to rapidly changing weather patterns and sea levels that are rising faster than the global average.

Rising water levels in the Yangtze River following intense rains in southern China have prompted eastern regions downstream to prepare for possible flooding.

Widespread seawater intrusions beneath the grounded ice of Thwaites Glacier, West Antarctica




We present evidence for seawater intrusions occurring at tidal frequencies over many kilometers beneath the grounded ice of Thwaites Glacier, West Antarctica, a major contributor to sea level rise. The results call into question the traditional approach of modeling a fixed, abrupt transition from grounded ice to ice floating in the ocean with no ice melt at the transition boundary. We delineate a tidally controlled grounding zone, 2 to 6 km in length, and additionally irregular seawater intrusions extending another 6 km inland at spring tide. The rushing of seawater beneath grounded ice over considerable distances makes the glacier more vulnerable to melting from a warmer ocean than anticipated, which in turn will increase projections of ice mass loss.




Warm water from the Southern Ocean has a dominant impact on the evolution of Antarctic glaciers and in turn on their contribution to sea level rise. Using a continuous time series of daily-repeat satellite synthetic-aperture radar interferometry data from the ICEYE constellation collected in March–June 2023, we document an ice grounding zone, or region of tidally controlled migration of the transition boundary between grounded ice and ice afloat in the ocean, at the main trunk of Thwaites Glacier, West Antarctica, a strong contributor to sea level rise with an ice volume equivalent to a 0.6-m global sea level rise. The ice grounding zone is 6 km wide in the central part of Thwaites with shallow bed slopes, and 2 km wide along its flanks with steep basal slopes. We additionally detect irregular seawater intrusions, 5 to 10 cm in thickness, extending another 6 km upstream, at high tide, in a bed depression located beyond a bedrock ridge that impedes the glacier retreat. Seawater intrusions align well with regions predicted by the GlaDS subglacial water model to host a high-pressure distributed subglacial hydrology system in between lower-pressure subglacial channels. Pressurized seawater intrusions will induce vigorous melt of grounded ice over kilometers, making the glacier more vulnerable to ocean warming, and increasing the projections of ice mass loss. Kilometer-wide, widespread seawater intrusion beneath grounded ice may be the missing link between the rapid, past, and present changes in ice sheet mass and the slower changes replicated by ice sheet models.