Here, we revisit our design process retrospectively using the SCORE* framework. The baseline workflow exhibits a key symptom: scientists (glaciologists) experienced high cognitive effort when attempting to analyse both spatial and temporal patterns in glacier dynamics (Vis-High-Ct, Int-High-Ct). The underlying cause is that existing visualizations separate the spatial and temporal dimensions into different representations, forcing analysts to integrate information mentally. This results in low alphabet compression and increased cognitive cost during the analytical process (Vis-Low-AC).
To address this issue, the design team introduced a remedy in the form of a radial visualization that integrates spatial and temporal information into a single representation (Vis-High-AC). The design leverages the geographical characteristic that glacier termini lie along the coastal boundary of Greenland. By treating the coastline as a one-dimensional boundary embedded in two-dimensional space, the visualization reduces the spatial dimension and maps glacier locations onto angular coordinates around a circle. Time is represented as concentric rings radiating outward from the centre, where each ring corresponds to a different year. This radial projection allows the visualization to display nearly 200 glacier time series simultaneously while preserving their spatial ordering along the coastline. This approach makes a shift from one suffering from Vis-Low-AC to one that increases Vis-High-AC to reduce Vis-High-Ct in the analytical process.
A naive radial mapping would project glaciers to a circle according to their original x-y positions. Because the coastal boundary is not convex, the correct order alone the coastal line is not assured. The cause of this issue is Vis-high-AC in terms of ordering. A side-effect of the remedy is thus that increasing Vis-High-AC risks introducing Vis-High-PD. This is likely due to the abstraction potentially impacting geographic relationships. In [3], the authors highlight how increases in alphabet compression often come with increased potential distortion, this is possibly an example of this trade-off.
This introduces a new symptom related to loss of geographic context. The cause is the distortion introduced by uniform angular mapping. To mitigate this issue, we developed a spatial mapping algorithm that preserves the natural ordering of glacier termini along the coastline. In a first step the algorithm snaps glacier positions to the coastal boundary, then computes traversal distances between neighbouring glaciers. These distances are then used to distribute the glaciers in angular space while maintaining neighbourhood relationships.
Despite this improvement, glaciers spatially tightly clustered can lead to densely packed radial axes and introduce overlapping or visual clutter (Vis-High-Ct, Vis-High-PD). To address this symptom, we introduced an angular relaxation algorithm enforcing a minimum spacing between neighbouring axes while maintaining key spatial reference points (Vis-Low-PD). These reference points correspond to glaciers located near cardinal directions (north, south, east, west), which serve as anchors for maintaining geographic orientation. While this relaxation process improves readability and reduces clutter, it introduces a small degree of spatial distortion, representing a typical trade-off between alphabet compression and pattern distortion within the framework [3].
A further challenge concerns the effective representation of glacier advance and retreat values. Colour-only encoding can make it difficult to distinguish magnitude and sign of changes, especially when galciologists compare multiple time steps (Vis-High-Ct). To overcome this limitation, the final visualization design, as shown in Figure 2, uses diverging colour schemes combined with geometric encoding. Positive values representing glacier advance are shown using blue tones, while negative values representing retreat are shown using red tones. The magnitude of change is represented through amplitude or thickness in radial stream-like plots. Two final visual styles were proposed: an area-based radial plot and a tube-style representation that emphasises magnitude through thickness (reducing Vis-High-Ct, while still maintaining sufficient Vis-High-AC for overview).