Climate during the Cretaceous was warmer than the present day, with reduced temperature gradients from the equator to poles. This 'greenhouse climate' led to high levels of humidity and precipitation.
The increased rainfall could have contributed to the flooding in several ways:
- Rivers carried more water and could have overflowed their banks more frequently, inundating adjacent lands.
- The saturated ground may have been unable to absorb additional rainfall, leading to surface runoff and flooding.
- Warm temperatures could enhance the hydrological cycle, thereby increasing the volume of water circulating through the atmosphere and falling as rain.
These climatic conditions, in conjunction with rising sea levels and tectonic shifts, created the perfect storm for widespread flooding during the Cretaceous period.