1. General comments:

- Concise review of regional wind wave scenarios in the North and Baltic Sea areas, focusing on the range of potential future changes.

- Uses state-of-the-art analysis methods, e.g. the ensemble approach and statistical significance tests.

- Analysis and results for average and higher wave events, considering spatial and temporal variability.

- Discusses the role of uncertainty in future projections.

The scientific methods and assumptions are clearly outlined, and the experiments and calculations are well described. It would be helpful to mention the sources of the regional climate model data, e.g. where the data was provided/downloaded from. This would facilitate reproduction by fellow scientists.

The author gives proper credit to related work in the field and indicates new contributions (see general comments).

The title accurately reflects the contents of the paper (see specific comments).

The abstract provides a concise and complete summary of the paper.

The overall presentation is well structured and clear, and the language is fluent and mostly correct (see technical corrections).

Abbreviations and units are used correctly.

Some minor aspects of the paper could be improved (see the specific comments).

The number and quality of references are appropriate.

The supplementary materials provided are appropriate.

2. Specific comments:

The changes in significant wave height are analysed and discussed. Changes in wave periods and directions are not analysed or discussed, even though these can also have important implications, e.g. for coastal erosion and flooding.

The limitation of the study to significant wave height should be clearer outlined, e.g. in the title or introduction.

The authors show that patterns of change may diverge depending on the statistical variable under consideration. The implications of climate change signals could be discussed in the 'Discussion' section. For example, a relative change in the ensemble median or the 99th percentile, or the maximum and with the same magnitude can have different implications.

3. Technical corrections:

L134: Replace the plural 'areas' with the singular.

L279: the word 'is' is missing before 'evident'.

The manuscript presents an updated and expanded ensemble assessment of future significant wave height (SWH) projections for the North Sea and Baltic Sea using CMIP3 and CMIP5-driven regional simulations. The study revisits earlier work and strengthens robustness through a larger ensemble and sub-ensemble comparison (high vs low emission scenarios). The topic is relevant and timely for regional coastal risk assessment and marine infrastructure planning. The ensemble-based framework and separation into emission categories are strengths. However, several methodological, clarity, and structural issues need attention before publication.

The manuscript only includes CMIP3 and CMIP5 simulations, while CMIP6 is now widely used. (1) Why were CMIP6 projections not incorporated? (2) Even if unavailable, this limitation must be clearly justified and discussed. (3) A comparison with recent CMIP6-based wave studies would strengthen the manuscript.

The ensemble includes 4 time-slice simulations and 10 transient simulations. The main Concerns are that these simulation types are methodologically different, with Time-slice experiments lacking transient internal variability representation. Secondly, Secodn the Mixing them in the same ensemble may introduce structural inconsistencies. The authors must justify combining both types (1) Assess whether results change when excluding time-slice runs.

The manuscript states that all ensemble members are treated as equally plausible. Issues: (1) Different GCM–RCM combinations have varying skill. (2) No performance-based weighting is applied. (3) No evaluation of historical skill for CMIP5-driven runs is shown.

While spatial patterns are described, physical mechanisms are only briefly discussed. Provide the detailed wind field change diagnostics, NAO influence discussion, Storm track shifts, Changes in cyclone intensity, Fetch and directional wave energy changes.