The absorption of energy by water vapour keeps the average temperature on Earth at a level that makes life possible. However, the average temperature increased in recent decades due to increased greenhouse gas emissions. This anthropogenic increase is amplified by the water vapour feedback. Water vapour is further an important component of the water cycle and indirectly of the energy cycle. The role of water vapour in these cycles in a changing climate needs to be fully understood and quantified. Thus, high-quality observations of water vapour and the characterisation and validation of associated uncertainties are of high importance for climate applications. Topics covered around atmospheric water vapour include, among others, retrieval development, data records, uncertainty characterisation and validation, inter-comparisons, climate applications, and model validation.

This special issue originates from the GEWEX Water Vapor Assessment (G-VAP, http://gewex-vap.org) and is open for all submissions within scope, not just from G-VAP.

In this special issue papers resulting from two major combined field campaigns shall be aggregated: (i) the Arctic CLoud Observations Using airborne measurements during polar Day (ACLOUD), and (ii) the Physical feedbacks of Arctic boundary layer, Sea ice, Cloud and AerosoL (PASCAL). These two concurrent campaigns took place in the vicinity of Svalbard in May and June 2017. They were designed to study processes important for explaining Arctic amplification, and, in particular, for investigating the role of microphysical and dynamical properties of Arctic low- and mid-level, mixed-phase clouds, and their interactions with atmospheric radiation and aerosol particles. Ground-based, ship-borne, tethered balloon, aircraft, and satellite observations have been combined. The research vessel (RV) Polarstern, an ice floe camp (erected close to the icebreaker) including an instrumented tethered balloon, and the two research aircraft, Polar 5 and Polar 6, were jointly operated. Polar 5 served as a mobile remote sensing observatory looking at the clouds from above, whereas Polar 6 operated as a flying in situ measurement laboratory mostly sampling inside the clouds. The permanent ground station of Ny-Ålesund observed the clouds from below, applying similar but upward-looking remote sensing equipment as Polar 5. Some of the flights were performed underneath respective satellite tracks. In this special issue we compile a number of papers reporting about the results of the observations conducted during ACLOUD/PASCAL within the framework of the (AC)³ project (http://www.ac3-tr.de/).

This special issue serves as a collection point for papers describing the datasets collected and developed during the "Elucidating the role of clouds–circulation coupling in climate" (EUREC4A) field campaign. This campaign, which served as an organizing umbrella for various complementary efforts such as the Atlantic Tradewind Ocean–Atmosphere Mesoscale Interaction Campaign (ATOMIC), was conducted in January and February of 2020 and took place in and over the tropical Atlantic Ocean around Barbados. These efforts involved broad international participation and the deployment of a wide array of observational platforms, including several research vessels, manned and robotic research aircraft, autonomous ocean samplers, enhanced satellite observations, and land-based observational capabilities. In addition, several groups produced specialized forecasting tools in support of campaign planning, and several others are in the process of preparing forcing datasets for numerical experiments that bridge a variety of scales. This special issue is envisioned to include invited and contributed papers related to the datasets developed as part of EUREC4A, ATOMIC, and related activities.

The Arctic, the Antarctic, and the Tibetan Plateau are called the three poles. Although the regions are geographically separated, they are often regarded as a group because of the similar extreme cryosphere environments and their critical role in maintaining Earth’s climate, hydrology, and ecosystem conditions. The three poles contain the world’s highest mountains and extreme environments and store more snow, ice, and freshwater than anywhere else in the world. However, the regions are found to be particularly sensitive to climate change, and their changes could also lead to critical feedback loops of global climate changes and the sustainability of human society. Unfortunately, our understanding of the three poles, especially the connections among the regions, is still limited. The spare and scattered data collected and produced for these harsh environments are one of the main bottlenecks for promoting comprehensive studies of the regions. With this special issue, we are looking forward to inviting experts to review and present existing and new datasets for the three poles region, to recognize these valuable datasets, and to promote their use in international and interdisciplinary studies of the three poles.

The glacial–interglacial cyclicity of the climate system varied in the past, most notably during the transition from a 40 ka to a 100 ka world in the mid-Pleistocene. Gases trapped in Antarctic ice are the most direct access available to investigate the composition of the paleo-atmosphere of that age and processes related to climate variability. The International Partnerships in Ice Core Sciences (IPICS) Oldest Ice endeavour aims at obtaining an undisturbed ice-core record older than 1 Ma. In addition to ice cores, time slices of paleo-records, available, for example, in Antarctic blue-ice fields, provide further valuable information, which complements continuous time series based on ice cores. This special issue will assemble contributions dedicated to the preparatory phase of this global effort to obtain ice samples and time series older than 700 000 years. This includes a consideration of glaciogical and geophysical settings which allow the presence of old ice, results from pre-site surveys and modelling studies, aspects of ice-core and other sampling techniques and analyses, and requirements for drilling and core handling.

This ESSD special issue addresses a need in the atmospheric chemistry and air quality modelling community for improved, detailed state-of-the-art, and high-resolution global and regional surface emission inventories. Surface emissions are used as input in chemistry transport models (CTMs) for air quality modelling, as well as in chemistry climate models which simulate atmospheric chemistry interactions and feedbacks (e.g. radiative direct and non-direct effects). Up-to-date and accurate estimates of these emissions, including as much spatial and temporal detail as possible, are necessary to drive these model simulations which are the basis for climate change assessment and mitigation strategies.

This initiative arises out of several concerted efforts within the atmospheric chemistry community to bring together such datasets. For example, CAMS_81, a funded project of the Copernicus Atmospheric Monitoring Service, is responsible for providing consistent and up-to-date global and regional emissions datasets that are used by the European Centre for Medium-Range Weather Forecast's chemical forecasting models and by many other CTMs within the CAMS systems. All contributions of original and openly available anthropogenic and natural surface emission datasets which support and promote research aimed towards understanding their impact on air quality and climate are welcome. Submissions are also encouraged from emission datasets that are constructed using alternative methods such as inverse modelling of satellite-derived atmospheric chemical concentrations. For the review process, contributors are encouraged to submit a representative subset of their data product for referees to browse their data without downloading the entire dataset. If possible, for consistency we ask that this data subset focus on the season DJF 2014/2015, although it is not a requirement.

Authors are invited to submit their data set(s) to the ECCAD (Emissions of atmospheric Compounds and Compilation of Ancillary Data) data repository ( https://eccad.aeris-data.fr/).

The development of the CAMS datasets included in this special issue has been funded by the Copernicus Atmosphere Monitoring Service, which is operated by the European Centre for Medium-Range Weather Forecasts on behalf of the European Commission as part of the Copernicus programme (http://copernicus.eu/).

The climate research community uses reanalyses widely to understand atmospheric processes and variability in the middle atmosphere, yet different reanalyses may give very different results for the same diagnostics. For example, the global energy budget and hydrological cycle, the Brewer–Dobson circulation, stratospheric vortex weakening and intensification events, and large-scale wave activity at the tropical tropopause are known to differ among reanalyses.

The Stratosphere–troposphere Processes And their Role in Climate (SPARC) Reanalysis Intercomparison Project (S-RIP) is a coordinated activity to compare reanalysis data sets with respect to a variety of key diagnostics. The objectives of this project are

1. to understand the causes of differences among reanalyses;
2. to provide guidance on the appropriate usage of various reanalysis products in scientific studies;
3. to contribute to future improvements in the reanalysis products by establishing collaborative links between the reanalysis centres and the SPARC community.

The project focuses predominantly on differences among reanalyses (although studies that include operational analyses are welcome and studies comparing reanalyses with observations are encouraged), with an emphasis on diagnostics in the upper troposphere, stratosphere and mesosphere. This special issue serves to collect research with relevance to S-RIP in preparation for the publication of the S-RIP report in 2018. Although participation in S-RIP is not a prerequisite for submission to this special issue, authors contributing to this collection are encouraged to consider contributing to the preparation of the S-RIP report.

The Water Vapour Phase II (WAVAS II), a SPARC activity, started in 2008 (SPARC Newsletter No. 30 (2008) p. 16: SPARC Water Vapour Initiative, by C. Schiller et al.). The activity includes satellite assessment and in situ comparison components. This international activity encompasses:

1) Providing a quality assessment of upper tropospheric to lower mesospheric satellite records since the early 1990s
2) Providing, as far as possible, absolute validation against ground-truth instruments
3) Assessing inter-instrument biases, depending on altitude, location, and season
4) Assessing the representation of temporal variations on various scales
5) Including data records on isotopologues
6) Providing recommendations for usage of available data records and for future observation systems


The main objective of WAVAS II is to assess and extend our knowledge and understanding of measurements of the vertical distribution of water vapor in the upper troposphere and middle atmosphere (UT/MA), where water has small concentrations, but significant radiative impact. This is a follow-up of the SPARC WAVAS activity, whose report was published in 2000 (SPARC Report No. 2 (2000) Upper Tropospheric and Stratospheric Water Vapour. D. Kley, J.M. Russell III, and C. Philips (eds.). WCRP-113, WMO/TD – No. 1043). Information gained from this activity will improve our ability to estimate long-term changes with associated uncertainties in UT/MA water as well as make recommendations as to what data would be most valuable for model validation and how such data should be used.

Papers will be accepted for this special issue according to the following guidelines, independent if they originate from the WAVAS II activity or other activities.

Guidelines for submissions:

• Papers covering existing UT/MA satellite water vapour measurements;
• Papers discussing comparisons of UT/MA satellite measurements, including discussion of quantities derived from these measurements, such as seasonal cycles, estimates of transport, or estimates of drifts, trends and variability.
• Papers discussing merging of water vapour measurements will be considered, although this topic is not specifically part of the WAVAS-II activity.
• Model papers that incorporate the datasets discussed and the uncertainty estimates resulting from the WAVAS-II activity will also be considered for inclusion.

The Arctic, the Antarctic, and the Tibetan Plateau are called the three poles. Although the regions are geographically separated, they are often regarded as a group because of the similar extreme cryosphere environments and their critical role in maintaining Earth’s climate, hydrology, and ecosystem conditions. The three poles contain the world’s highest mountains and extreme environments and store more snow, ice, and freshwater than anywhere else in the world. However, the regions are found to be particularly sensitive to climate change, and their changes could also lead to critical feedback loops of global climate changes and the sustainability of human society. Unfortunately, our understanding of the three poles, especially the connections among the regions, is still limited. The spare and scattered data collected and produced for these harsh environments are one of the main bottlenecks for promoting comprehensive studies of the regions. With this special issue, we are looking forward to inviting experts to review and present existing and new datasets for the three poles region, to recognize these valuable datasets, and to promote their use in international and interdisciplinary studies of the three poles.

The absorption of energy by water vapour keeps the average temperature on Earth at a level that makes life possible. However, the average temperature increased in recent decades due to increased greenhouse gas emissions. This anthropogenic increase is amplified by the water vapour feedback. Water vapour is further an important component of the water cycle and indirectly of the energy cycle. The role of water vapour in these cycles in a changing climate needs to be fully understood and quantified. Thus, high-quality observations of water vapour and the characterisation and validation of associated uncertainties are of high importance for climate applications. Topics covered around atmospheric water vapour include, among others, retrieval development, data records, uncertainty characterisation and validation, inter-comparisons, climate applications, and model validation.

This special issue originates from the GEWEX Water Vapor Assessment (G-VAP, http://gewex-vap.org) and is open for all submissions within scope, not just from G-VAP.

This special issue serves as a collection point for papers describing the datasets collected and developed during the "Elucidating the role of clouds–circulation coupling in climate" (EUREC4A) field campaign. This campaign, which served as an organizing umbrella for various complementary efforts such as the Atlantic Tradewind Ocean–Atmosphere Mesoscale Interaction Campaign (ATOMIC), was conducted in January and February of 2020 and took place in and over the tropical Atlantic Ocean around Barbados. These efforts involved broad international participation and the deployment of a wide array of observational platforms, including several research vessels, manned and robotic research aircraft, autonomous ocean samplers, enhanced satellite observations, and land-based observational capabilities. In addition, several groups produced specialized forecasting tools in support of campaign planning, and several others are in the process of preparing forcing datasets for numerical experiments that bridge a variety of scales. This special issue is envisioned to include invited and contributed papers related to the datasets developed as part of EUREC4A, ATOMIC, and related activities.

This ESSD special issue addresses a need in the atmospheric chemistry and air quality modelling community for improved, detailed state-of-the-art, and high-resolution global and regional surface emission inventories. Surface emissions are used as input in chemistry transport models (CTMs) for air quality modelling, as well as in chemistry climate models which simulate atmospheric chemistry interactions and feedbacks (e.g. radiative direct and non-direct effects). Up-to-date and accurate estimates of these emissions, including as much spatial and temporal detail as possible, are necessary to drive these model simulations which are the basis for climate change assessment and mitigation strategies.

This initiative arises out of several concerted efforts within the atmospheric chemistry community to bring together such datasets. For example, CAMS_81, a funded project of the Copernicus Atmospheric Monitoring Service, is responsible for providing consistent and up-to-date global and regional emissions datasets that are used by the European Centre for Medium-Range Weather Forecast's chemical forecasting models and by many other CTMs within the CAMS systems. All contributions of original and openly available anthropogenic and natural surface emission datasets which support and promote research aimed towards understanding their impact on air quality and climate are welcome. Submissions are also encouraged from emission datasets that are constructed using alternative methods such as inverse modelling of satellite-derived atmospheric chemical concentrations. For the review process, contributors are encouraged to submit a representative subset of their data product for referees to browse their data without downloading the entire dataset. If possible, for consistency we ask that this data subset focus on the season DJF 2014/2015, although it is not a requirement.

Authors are invited to submit their data set(s) to the ECCAD (Emissions of atmospheric Compounds and Compilation of Ancillary Data) data repository ( https://eccad.aeris-data.fr/).

The development of the CAMS datasets included in this special issue has been funded by the Copernicus Atmosphere Monitoring Service, which is operated by the European Centre for Medium-Range Weather Forecasts on behalf of the European Commission as part of the Copernicus programme (http://copernicus.eu/).

In this special issue papers resulting from two major combined field campaigns shall be aggregated: (i) the Arctic CLoud Observations Using airborne measurements during polar Day (ACLOUD), and (ii) the Physical feedbacks of Arctic boundary layer, Sea ice, Cloud and AerosoL (PASCAL). These two concurrent campaigns took place in the vicinity of Svalbard in May and June 2017. They were designed to study processes important for explaining Arctic amplification, and, in particular, for investigating the role of microphysical and dynamical properties of Arctic low- and mid-level, mixed-phase clouds, and their interactions with atmospheric radiation and aerosol particles. Ground-based, ship-borne, tethered balloon, aircraft, and satellite observations have been combined. The research vessel (RV) Polarstern, an ice floe camp (erected close to the icebreaker) including an instrumented tethered balloon, and the two research aircraft, Polar 5 and Polar 6, were jointly operated. Polar 5 served as a mobile remote sensing observatory looking at the clouds from above, whereas Polar 6 operated as a flying in situ measurement laboratory mostly sampling inside the clouds. The permanent ground station of Ny-Ålesund observed the clouds from below, applying similar but upward-looking remote sensing equipment as Polar 5. Some of the flights were performed underneath respective satellite tracks. In this special issue we compile a number of papers reporting about the results of the observations conducted during ACLOUD/PASCAL within the framework of the (AC)³ project (http://www.ac3-tr.de/).

The Water Vapour Phase II (WAVAS II), a SPARC activity, started in 2008 (SPARC Newsletter No. 30 (2008) p. 16: SPARC Water Vapour Initiative, by C. Schiller et al.). The activity includes satellite assessment and in situ comparison components. This international activity encompasses:

1) Providing a quality assessment of upper tropospheric to lower mesospheric satellite records since the early 1990s
2) Providing, as far as possible, absolute validation against ground-truth instruments
3) Assessing inter-instrument biases, depending on altitude, location, and season
4) Assessing the representation of temporal variations on various scales
5) Including data records on isotopologues
6) Providing recommendations for usage of available data records and for future observation systems


The main objective of WAVAS II is to assess and extend our knowledge and understanding of measurements of the vertical distribution of water vapor in the upper troposphere and middle atmosphere (UT/MA), where water has small concentrations, but significant radiative impact. This is a follow-up of the SPARC WAVAS activity, whose report was published in 2000 (SPARC Report No. 2 (2000) Upper Tropospheric and Stratospheric Water Vapour. D. Kley, J.M. Russell III, and C. Philips (eds.). WCRP-113, WMO/TD – No. 1043). Information gained from this activity will improve our ability to estimate long-term changes with associated uncertainties in UT/MA water as well as make recommendations as to what data would be most valuable for model validation and how such data should be used.

Papers will be accepted for this special issue according to the following guidelines, independent if they originate from the WAVAS II activity or other activities.

Guidelines for submissions:

• Papers covering existing UT/MA satellite water vapour measurements;
• Papers discussing comparisons of UT/MA satellite measurements, including discussion of quantities derived from these measurements, such as seasonal cycles, estimates of transport, or estimates of drifts, trends and variability.
• Papers discussing merging of water vapour measurements will be considered, although this topic is not specifically part of the WAVAS-II activity.
• Model papers that incorporate the datasets discussed and the uncertainty estimates resulting from the WAVAS-II activity will also be considered for inclusion.

The climate research community uses reanalyses widely to understand atmospheric processes and variability in the middle atmosphere, yet different reanalyses may give very different results for the same diagnostics. For example, the global energy budget and hydrological cycle, the Brewer–Dobson circulation, stratospheric vortex weakening and intensification events, and large-scale wave activity at the tropical tropopause are known to differ among reanalyses.

The Stratosphere–troposphere Processes And their Role in Climate (SPARC) Reanalysis Intercomparison Project (S-RIP) is a coordinated activity to compare reanalysis data sets with respect to a variety of key diagnostics. The objectives of this project are

1. to understand the causes of differences among reanalyses;
2. to provide guidance on the appropriate usage of various reanalysis products in scientific studies;
3. to contribute to future improvements in the reanalysis products by establishing collaborative links between the reanalysis centres and the SPARC community.

The project focuses predominantly on differences among reanalyses (although studies that include operational analyses are welcome and studies comparing reanalyses with observations are encouraged), with an emphasis on diagnostics in the upper troposphere, stratosphere and mesosphere. This special issue serves to collect research with relevance to S-RIP in preparation for the publication of the S-RIP report in 2018. Although participation in S-RIP is not a prerequisite for submission to this special issue, authors contributing to this collection are encouraged to consider contributing to the preparation of the S-RIP report.

The glacial–interglacial cyclicity of the climate system varied in the past, most notably during the transition from a 40 ka to a 100 ka world in the mid-Pleistocene. Gases trapped in Antarctic ice are the most direct access available to investigate the composition of the paleo-atmosphere of that age and processes related to climate variability. The International Partnerships in Ice Core Sciences (IPICS) Oldest Ice endeavour aims at obtaining an undisturbed ice-core record older than 1 Ma. In addition to ice cores, time slices of paleo-records, available, for example, in Antarctic blue-ice fields, provide further valuable information, which complements continuous time series based on ice cores. This special issue will assemble contributions dedicated to the preparatory phase of this global effort to obtain ice samples and time series older than 700 000 years. This includes a consideration of glaciogical and geophysical settings which allow the presence of old ice, results from pre-site surveys and modelling studies, aspects of ice-core and other sampling techniques and analyses, and requirements for drilling and core handling.