In the era of water scarcity and severe droughts, the accurate estimation of
evapotranspiration (ET) is crucial for the efficient management of water resources …

The Earth's climate is largely determined by its energy budget. Since the 1960s, satellite
remote sensing has been used in estimating these energy budget components at both the …

The carbon sequestration capacity of alpine grasslands, composed of alpine meadows and
steppes, in the Tibetan Plateau has an essential role in regulating the regional carbon cycle …

Actual evapotranspiration (ET) plays a key role in the water cycle and energy balance, and it
is also sensitive to climate and land use changes due to its explicit link with multiple land …

Terrestrial evapotranspiration (ET a) reflects the complex interactions of climate, vegetation,
soil and terrain and is a critical component in water and energy cycles. However, the manner …

Evapotranspiration (ET) exerts substantial effects on terrestrial ecosystem carbon and water
cycles. A deep understanding of the spatial and temporal variability in ET and its dominant …

Terrestrial evapotranspiration (ET) refers to a key process in the hydrological cycle by which
water is transferred from the Earth's surface to lower atmosphere. With spatiotemporal …

Re-vegetation is a necessary control measure of soil erosion in the Loess Plateau. However,
excessive re-vegetation can aggravate soil water shortage, which can in turn threaten the …

Global warming intensifies the water cycle and regional water condition differences by
changing the surface environment. The ecological system in environmental sensitive areas …

More accurate and process-based satellite evapotranspiration (ET) estimation for the
Tibetan Plateau (TP)—the Third Pole of the world—have long been of major interest in …