4D-Var Inversion of European NH3 Emissions Using CrIS NH3 Measurements and GEOS-Chem Adjoint With Bi-Directional and

Hansen Cao1, Daven K Henze1, Liye Zhu2

  • 1University of Colorado Boulder CO USA.

Journal of Geophysical Research. Atmospheres : JGR
|July 22, 2022
PubMed
Summary

This study used satellite data and advanced modeling to better understand ammonia emissions in Europe. The researchers developed a new method that accounts for how ammonia moves between the air and surfaces. They found that their approach produces different seasonal patterns compared to previous estimates. Their results suggest that ammonia emissions in central Europe may be lower than previously thought. The study also shows that the way ammonia is modeled significantly affects emission estimates. The researchers found that their method better matches ground measurements, especially for daily patterns. Their results could help improve air quality policies. The study highlights the need for better satellite data to track ammonia's daily changes.

Frequently Asked Questions

Related Concept Videos

Inorganic Nitrogen Assimilation01:22

Inorganic Nitrogen Assimilation

Nitrogen is an essential element in biological systems, forming a crucial component of proteins, nucleic acids, and other cellular constituents. Many bacteria and archaea acquire nitrogen in the form of nitrate (NO₃⁻) or ammonia (NH₃), which are then assimilated into biomolecules through specific enzymatic pathways.Assimilatory Nitrate ReductionWhen nitrate enters the cell, it undergoes a two-step reduction process known as assimilatory nitrate reduction. Initially, the enzyme...
93
Free Energy Changes for Nonstandard States03:25

Free Energy Changes for Nonstandard States

The free energy change for a process taking place with reactants and products present under nonstandard conditions (pressures other than 1 bar; concentrations other than 1 M) is related to the standard free energy change according to this equation:
 
where R is the gas constant (8.314 J/K·mol), T is the absolute temperature in kelvin, and Q is the reaction quotient. This equation may be used to predict the spontaneity of a process under any given set of conditions.
Reaction Quotient...
11.6K
Isochoric and Isobaric Processes01:21

Isochoric and Isobaric Processes

A thermodynamic process that occurs at constant volume is called an isochoric process. According to the first law of thermodynamics, heat supplied or removed from the system is partially utilized to perform work and change the internal energy of the system. However, in an isochoric process, the volume remains constant. Hence, the work done by the system is zero. Therefore, the exchange of heat changes the internal energy of the system only. 
Suppose 1000 g of water is heated from 40...
3.6K