Carbon dioxide (CO2) is the primary greenhouse gas contributing to global warming and the associated impacts on coastal erosion.

The rise in global temperatures contributes to coastal erosion through various mechanisms, including melting of glaciers and ice sheets, leading to sea-level rise; increased frequency and intensity of storms, resulting in more powerful waves; and changes in ocean currents, causing altered sediment transport patterns.

Sea-level rise is the primary factor influencing the rate of coastal erosion, as it directly affects the position of the shoreline and the exposure of coastal land to wave energy.

Sea-level rise contributes to coastal erosion through multiple mechanisms, including increasing the depth of water near the shoreline, submerging coastal land, and altering sediment transport patterns, all of which make coastal areas more susceptible to wave attack and erosion.

Sandy beaches, coral reefs, mangrove forests, and salt marshes are all coastal landforms that are particularly vulnerable to erosion due to climate change, as they are directly exposed to wave energy and sea-level rise.

The loss of coastal land due to erosion has significant impacts on human communities, including loss of property and infrastructure, displacement of coastal populations, and increased risk of flooding and storm damage.

Adaptation strategies to mitigate the impacts of coastal erosion due to climate change include building seawalls and other hard structures to protect the shoreline, restoring and protecting natural coastal ecosystems, and implementing managed retreat strategies to relocate coastal communities away from vulnerable areas.

The Paris Agreement is an international agreement that aims to address climate change and its impacts, including coastal erosion, by setting targets for reducing greenhouse gas emissions and promoting adaptation measures.

Coastal vegetation, such as mangrove forests and salt marshes, plays a crucial role in mitigating coastal erosion by acting as natural buffers against waves and storm surges, stabilizing sediments and preventing erosion, and providing habitat for marine life and supporting biodiversity.

Climate change is leading to an increase in the frequency and intensity of coastal storms, such as hurricanes and cyclones, due to warmer ocean temperatures and changes in atmospheric circulation patterns.

Climate change primarily contributes to coastal erosion through increased sea level rise, which is caused by the melting of glaciers and ice sheets and the thermal expansion of ocean water.

Climate change can lead to decreased sediment supply to coastal areas due to changes in sediment transport patterns, reduced sediment availability from rivers, and increased erosion of coastal landforms.

Coastal erosion due to climate change is associated with negative consequences such as loss of coastal property and infrastructure, increased flooding and storm damage, and displacement of coastal communities. Improved water quality is not a typical consequence of coastal erosion.

Managed retreat is the term used to describe the process of relocating coastal communities away from vulnerable areas due to coastal erosion and sea-level rise. It involves planning and implementing strategies to move people and infrastructure away from at-risk locations.

Increasing greenhouse gas emissions is not a potential adaptation strategy to address coastal erosion due to climate change. Adaptation strategies aim to reduce the vulnerability of coastal areas to erosion and sea-level rise, while increasing greenhouse gas emissions would exacerbate the problem.