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2007
2017
2025
2024
2025
Absorpsjonslinjer i solspektra fylles igjen på grunn av rotasjonell Raman spredning (RRS). Ved analyse av UV og synlige spektra blir RRS rutinemessig korrigert for. Effekten er også tilstede ved lengre bølgelengder, men generelt avtar den når bølgelengdene øker. For spektra med høy spektraloppløsning kan effekten være av betydning. Avhengig av anvendelsen kan det være nødvendig å kvantifisere og korrigere for RRS også ved lengre bølgelengder. Av spesiell interesse er effekten i O2-A (759-769 nm) og O2-B (686-697 nm) bandene. Effekten av RRS i disse bandene blir presentert for satellittinstrumentene CarbonSat, FLEX/FLORIS, MERIS og OLCI.
2012
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2012
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2019
Robust evidence for reversal of the trend in aerosol effective climate forcing
Anthropogenic aerosols exert a cooling influence that offsets part of the greenhouse gas warming. Due to their short tropospheric lifetime of only several days, the aerosol forcing responds quickly to emissions. Here, we present and discuss the evolution of the aerosol forcing since 2000. There are multiple lines of evidence that allow us to robustly conclude that the anthropogenic aerosol effective radiative forcing (ERF) – both aerosol–radiation interactions (ERFari) and aerosol–cloud interactions (ERFaci) – has become less negative globally, i.e. the trend in aerosol effective radiative forcing changed sign from negative to positive. Bottom-up inventories show that anthropogenic primary aerosol and aerosol precursor emissions declined in most regions of the world; observations related to aerosol burden show declining trends, in particular of the fine-mode particles that make up most of the anthropogenic aerosols; satellite retrievals of cloud droplet numbers show trends in regions with aerosol declines that are consistent with these in sign, as do observations of top-of-atmosphere radiation. Climate model results, including a revised set that is constrained by observations of the ocean heat content evolution show a consistent sign and magnitude for a positive forcing relative to the year 2000 due to reduced aerosol effects. This reduction leads to an acceleration of the forcing of climate change, i.e. an increase in forcing by 0.1 to 0.3 W m−2, up to 12 % of the total climate forcing in 2019 compared to 1750 according to the Intergovernmental Panel on Climate Change (IPCC).
2022
A strategy for how Norwegian applied organizations should prepare for the upcoming EarthCARE and Sentinel 5 precursor satellite missions is discussed, and long- and short-term plans are provided. The satellites and their potential products are discussed in terms of possible applications by NILU and met.no and data are considered for operational use in (a) reporting of climate gases, aerosols, ozone and UV to Klif, (b) EMEP reporting on aerosol and acidification/eutrophication, (c) chemical weather forecasting, (d) numerical weather forecasting and (e) research on Cloud-Aerosol-Radiation interaction.
2011