Periodic Reporting for period 3 - UpTrop (Fundamental understanding of reactive nitrogen in the global upper troposphere)
Reporting period: 2022-02-01 to 2023-07-31
Though the upper troposphere is far away (8-12 km overhead), it is an important contributor to the quality of the air we breathe and it also affects the formation and persistence of climate-altering greenhouse gases. Without a clear understanding of the processes occurring in the upper troposphere, we are unable to develop well-informed policies that improve air quality and curtail a climate emergency.
The overarching objective of UpTrop is to address gaps in observations and knowledge of the processes occurring in the upper troposphere and use this new knowledge to determine the true influence of the upper troposphere on Earth’s atmosphere. We will achieve this using innovative data derivation techniques, rigorous statistical methods, state-of-art models, and recently launched space-based instruments with unprecedented spatial resolution.
The datasets and software that have been generated as part of UpTrop are available for public access and use (Data: https://doi.org/10.5522/04/14586558 https://doi.org/10.5522/04/17032349; Software: https://doi.org/10.5281/zenodo.4058442). It is evident from the number of people who have viewed (854) and downloaded (661) these, that UpTrop is producing highly sought after resources.
The UpTrop team is currently using these new datasets to determine how large the errors are in our understanding of the chemical composition of the upper troposphere by comparison to a state-of-art chemical transport model. The discrepancies we are identifying between the model and UpTrop datasets is guiding our further steps to investigate the causes for these differences.
Expected results at the end of UpTrop include publicly available datasets of atmospheric composition in the global upper troposphere, renewed understanding of the sources and physical and chemical processes that determine atmospheric composition in the global upper troposphere, improved constraints on important atmospheric sources of reactive nitrogen such as lightning, and greater confidence in the role of the upper troposphere in influencing Earth’s climate and air quality.