# River temperature response to atmospheric heatwaves is modulated by discharge and meltwater

## TL;DR

Alpine rivers don't always heat up during heatwaves due to factors like water flow and meltwater.

## Contribution

The study reveals that discharge and meltwater modulate river temperature responses to atmospheric heatwaves.

## Key findings

- Only 47% of atmospheric heatwaves result in riverine heatwaves.
- High discharge and meltwater prevent riverine heatwaves.
- Low discharge strengthens the air-river temperature link.

## Abstract

Alpine rivers are becoming increasingly exposed to atmospheric heatwaves. Because of their strong relationship with air temperature, rivers can experience persistent heat anomalies, known as riverine heatwaves, which can have serious consequences for river ecosystems and the economy. This study aims to improve our understanding of how river water temperature responds to atmospheric heatwaves by focusing on the interplay of various hydro-climatic variables that can strengthen or weaken the thermal sensitivity of rivers to such events. Our results show that the response of water temperature to atmospheric heatwaves can vary substantially, with only 47% of atmospheric heatwaves leading to riverine heatwaves. Riverine heatwave development can be prevented by positive anomalies in discharge and meltwater, while negative anomalies in discharge strengthen the link between atmospheric and river temperatures. Future changes in these hydro-climatic conditions will likely increase the sensitivity of Alpine rivers to atmospheric heatwaves.

Only half of atmospheric heatwaves trigger riverine ones because high discharge and meltwater act as buffers while low discharge strengthens the air-river temperature link, according to water temperature and discharge observations from 275 Alpine catchments.