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Le fa-introngen08 2014
No Slide Title Introduction to remote sensing and Earth observation NGEN08 NGEN09 EXTN15 Lars Eklundh Remote sensing / Earth observation Remote sensing: All collection of data at a distance, e.g. - Aerial photographs - Satellite data - Radar and Lidar (laser) from the ground and from the air Earth observation (EO): remote sensing of the Earth's surface Why use remote sensing? • Cover large area. M
https://www.nateko.lu.se/sv/sites/nateko.lu.se.sv/files/le_fa-introngen08_2014.pdf - 2026-05-30
The effect of relative humidity on eddy covariance latent heat flux measurements and its implication for partitioning into transpiration and evaporation
While the eddy covariance (EC) technique is a well-established method for measuring water fluxes (i.e., evaporation or 'evapotranspiration’, ET), the measurement is susceptible to many uncertainties. One such issue is the potential underestimation of ET when relative humidity (RH) is high (>70%), due to low-pass filtering with some EC systems. Yet, this underestimation for different types of EC sy
A comparative study on methanol and n-dodecane spray flames using Large-Eddy Simulation
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The Image of Climate Change. On Organisational Cognition and Responses
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Kp SMMV26 eng VT26 rev 250829
Taking the pulse of Earth's tropical forests using networks of highly distributed plots
Tropical forests are the most diverse and productive ecosystems on Earth. While better understanding of these forests is critical for our collective future, until quite recently efforts to measure and monitor them have been largely disconnected. Networking is essential to discover the answers to questions that transcend borders and the horizons of funding agencies. Here we show how a global commun