North America

Creative Rationale

Over the southeastern shores of Hudson Bay in northern Quebec, a moderate low pressure system churns with steady westerly winds and near-saturated air. The significant pressure gradient of 22.84 Pa/cell creates dense archaeological layers in this composition, while the 4.8°C temperature anomaly introduces fragmentary chaos breaking through more structured painted fields. The high humidity allows deep palimpsest visibility, with earlier gestural marks from the 7.5 m/s westerly wind energy showing through translucent upper layers, punctuated by subtle drip marks from the light precipitation that suggest years of reworking and weathering.