ATM-METFIN · Quantifying atmospheric ice nucleating particle (INP) concentrations via advances in measurement techniques and field studies of ice nucleation
„Хоризонт 2020“ — Действия „Мария Склодовска-Кюри“
- Период
- 2017-05-01 → 2019-04-30
- Финансиране от ЕС
- 175 420 €
- Участници
- 1
- Схема
- MSCA-IF
Линиите свързват координатора с партньорите.
Накратко на български
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Кратко обяснение, генерирано от езиков модел по текста на CORDIS. Оригиналът е по-долу.
Резултати накратко
Quantifying atmospheric ice nucleating particle (INP) concentrations via advances in measurement techniques and field studies of ice nucleation
Atmospheric aerosol particles play an important role in the global climate by way of influencing Earth’s hydrological cycle, energy and radiation balance. Due to their importance, aerosol-cloud interactions have been a subject of intense research over the last several decades. Despite that, exact quantification of aerosol effects on the changing cloud properties and the ability to predict future climate based on expected changes to global aerosol burden have been challenging. Ubiquitous in the atmosphere, atmospheric aerosol particles can participate in the formation of liquid and ice clouds by acting as cloud condensation nuclei (CCN) and ice nucleating particles (INPs), respectively. Both have received a lot of attention in recent years, with a multitude of studies attempting to quantify the importance of aerosols in the aerosol-cloud-climate system. The objectives of the project included the quantification of ice nucleating particles in condensation/immersion freezing modes under mixed-phase cloud conditions, the comparison to previously published data from other locations around the globe, the investigation of INP physical and chemical properties and the identification of the already known INP species in the boreal environment. The main results presented several important questions and conclusions for future ambient INP studies. First and foremost, it was not possible to identify physical and chemical properties of ambient INPs despite the complexity of instrumental setup and a multitude of additional instrumentations deployed during the campaign. Unfortunately, the current instrumental setup coupled with the rarity of ambient INPs rendered any speculations about INP identity inconclusive. If the future INP field studies aim to explicitly identify the physical and chemical properties of INPs, a single-particle analysis of ice crystal residuals must be carried out. The second important question that needs to be addressed as a result of this work is the necessity for future INP measurements. Future ambient INP studies need to explicitly focus on the physical and chemical properties of the INPs and whether they are different from the rest of the aerosol population. Additionally, future studies should aim to assess whether the explicit physics and chemistry of INPs can be and need to be parameterised in order to understand aerosol-cloud interactions on the global scale.
Текст от CORDIS, на английски · Данни: CORDIS, © Европейски съюз
Цел на проекта
The focal point of the research proposal is to combine the current technological advancement and scientific questions regarding the unknowns of atmospheric ice nucleation. Ice nucleation is an important pathway for cloud formation and initiation of precipitation, therefore playing a significant role in the Earth’s hydrological cycle and energy and radiative balance. Several questions pertinent to ice nucleation remain unanswered, partially due to gaps in instrumental technology and lack of ambient measurements. The proposed work primarily focuses on the mechanisms of ice nucleation in the atmosphere, more specifically the number, physics and chemistry of biogenic and anthropogenic aerosol particles able to act as ice nucleating particles (INP). Field measurements with technological improvements to the existing Portable Ice Nucleation Chamber (PINC) are planned. One of the goals is to continue the time series measurements of INP parameters at the Izaña Observatory in Tenerife, where measurements have been ongoing since 2013 by the host institution. Since the INP concentration exponentially decreases with increasing temperature, and it is the warmer sub-zero temperatures that are more relevant for the initial ice formation in mixed-phase, the goal is to extend the measurements of INP parameters at the Izaña Observatory in Tenerife to temperatures above −30°C. Using additional instrumentation in the field, the role of mineral dust, particles of anthropogenic origin and marine primary biogenic particles as potential INP will be investigated in more detail. From a technical perspective, the work will concentrate on lowering the detection limits of PINC and on improving its ability to differentiate between water droplets and ice crystals. These improvements will allow measuring INP at warmer sub-zero temperatures and in immersion/condensation mode, both of which are more relevant for the first ice formation in supercooled clouds than our current measurements.
Оригинален текст от CORDIS (на английски).
Участници
- EIDGENOESSISCHE TECHNISCHE HOCHSCHULE ZUERICH · ZuerichКоординаторШвейцария
Връзки
Данни: CORDIS, © Европейски съюз
