scholarly journals Photoacoustics: A Potent Tool for the Study of Energy Fluxes in Photosynthesis Research

10.5772/31159 ◽  
2012 ◽  
Author(s):  
Yulia Pinchasov-Grinblat ◽  
Zvy Dubinsky
Keyword(s):  
Energy Fluxes ◽  
Photosynthesis Research

ALGAE AND PROGRESS IN PHOTOSYNTHESIS RESEARCH I-Oxygen evolution and carbon fixation

2000 ◽  
Vol 1 (1) ◽  
pp. 235-244
Author(s):  
Ahmed Hamad ◽  
Mohamed Osman ◽  
Refaat Abdel-Basset
Keyword(s):  
Oxygen Evolution ◽  
Carbon Fixation ◽  
Photosynthesis Research

Photosynthesis research under climate change

2021 ◽  
Author(s):  
Sajad Hussain ◽  
Zaid Ulhassan ◽  
Marian Brestic ◽  
Marek Zivcak ◽  
Weijun Zhou ◽  
...  
Keyword(s):  
Climate Change ◽  
Photosynthesis Research

Understanding water and energy fluxes in the Amazonia: Lessons from an observation‐model intercomparison

2021 ◽  
Vol 27 (9) ◽  
pp. 1802-1819
Author(s):  
Natalia Restrepo‐Coupe ◽  
Loren P. Albert ◽  
Marcos Longo ◽  
Ian Baker ◽  
Naomi M. Levine ◽  
...  
Keyword(s):  
Observation Model ◽  
Model Intercomparison ◽  
Energy Fluxes

scholarly journals Comparison of FASST and SNTHERM in Three Snow Accumulation Regimes

2008 ◽  
Vol 9 (6) ◽  
pp. 1443-1463 ◽  
Author(s):  
Susan Frankenstein ◽  
Anne Sawyer ◽  
Julie Koeberle
Keyword(s):  
Surface Energy ◽  
Single Layer ◽  
Soil Strength ◽  
Snow Accumulation ◽  
Dynamic State ◽  
Energy Fluxes ◽  
One Dimensional ◽  
Surface Energy Fluxes ◽  
Snow Model ◽  
Surface Ice

Abstract Numerical experiments of snow accumulation and depletion were carried out as well as surface energy fluxes over four Cold Land Processes Experiment (CLPX) sites in Colorado using the Snow Thermal model (SNTHERM) and the Fast All-Season Soil Strength model (FASST). SNTHERM is a multilayer snow model developed to describe changes in snow properties as a function of depth and time, using a one-dimensional mass and energy balance. The model is intended for seasonal snow covers and addresses conditions found throughout the winter, from initial ground freezing in the fall to snow ablation in the spring. It has been used by many researchers over a variety of terrains. FASST is a newly developed one-dimensional dynamic state-of-the-ground model. It calculates the ground’s moisture content, ice content, temperature, and freeze–thaw profiles as well as soil strength and surface ice and snow accumulation/depletion. Because FASST is newer and not as well known, the authors wanted to determine its use as a snow model by comparing it with SNTHERM, one of the most established snow models available. It is demonstrated that even though FASST is only a single-layer snow model, the RMSE snow depth compared very favorably against SNTHERM, often performing better during the accumulation phase. The surface energy fluxes calculated by the two models were also compared and were found to be similar.

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