Results for "climate adaptation"
Sea Level Rise
** Sea level rise is the long‑term increase in the average height of the world’s oceans, driven primarily by human‑induced climate change and manifesting as faster, more widespread coastal impacts than any period in the past several millennia. **CONTENT:** ## Overview Sea level rise (SLR) refers to the **gradual increase in the mean height of the world’s oceans** relative to land. While the oceans have been slowly climbing since the end of the **Last Glacial Maximum** (~20 000 years ago), the pace of rise has accelerated dramatically in the modern era. Between **1901 and 2018**, global mean sea level (GMSL) rose by **15–25 cm (6–10 in)**, averaging **2.3 mm yr⁻¹** since the 1970s. The most recent decade (2013–2022) saw an even steeper climb of **4.62 mm yr⁻¹**, a rate that outpaces any sustained increase documented over the past **3 000 years**. The primary drivers are **thermal expansion**—the tendency of seawater to occupy more volume as it warms—and the **melting of glaciers and ice sheets**. Between **1993 and 2018**, melting contributed roughly **44 %** of observed SLR, while thermal expansion accounted for about **42 %**. The remaining fraction stems from changes in land water storage, such as groundwater extraction and reservoir impoundment. Rising seas reshape coastlines, erode beaches, inundate low‑lying islands, and amplify storm surge impacts. For ecosystems, saltwater intrusion threatens freshwater wetlands, mangroves, and coral reefs, while human societies confront heightened flood risk, displacement, and costly infrastructure adaptation. ## History/Background The story of sea level rise begins with the **Last Glacial Maximum**, when massive ice sheets locked away roughly **30 %** of Earth’s water, leaving sea levels about **120 m (394 ft)** lower than today. As the climate warmed, these ice sheets melted, initiating a multi‑millennial rise that slowed around **7 000 years ago** when the planet entered the relatively stable **Holocene** epoch. In the **19th century**, systematic tide‑gauge networks began recording sea level, revealing a modest upward trend. The **20th century** witnessed a noticeable uptick: from **1901 to 1970**, the rise averaged **~1.5 mm yr⁻¹**. Post‑1970, industrial emissions of **CO₂** and other greenhouse gases accelerated global warming, pushing the rate to **2.3 mm yr⁻¹**. Satellite altimetry, launched in **1992**, provided precise, global measurements, confirming the acceleration and exposing regional variability linked to ocean currents and gravitational effects of melting ice. Key dates: - **1970s** – Global mean sea level begins rising at >2 mm yr⁻¹. - **1992** – Launch of TOPEX/Poseidon satellite, enabling high‑resolution sea‑level monitoring. - **2013–2022** – Decadal average climbs to **4.62 mm yr⁻¹**, the fastest sustained rate in the instrumental record. ## Key Information - **Magnitude (1901‑2018):** 15–25 cm (6–10 in) global average. - **Current rate (2013‑2022):** 4.62 mm yr⁻¹ (0.182 in/yr). - **Drivers (1993‑2018):** - **Ice melt:** 44 % (Greenland, Antarctica, mountain glaciers). - **Thermal expansion:** 42 % (warming of the upper ocean layers). - **Land water storage changes:** ~14 %. - **Projected rise (2100):** IPCC AR6 scenarios range from **0.28 m** (low‑emissions) to **0.86 m** (high‑emissions) above 2000 levels. - **Regional hotspots:** The western Pacific, Gulf of Mexico, and parts of the North Atlantic experience amplified rise due to ocean dynamics and land subsidence. - **Ecological impacts:** Saltwater intrusion into estuaries, loss of **mangrove forests**, increased stress on **coral reefs**, and altered migratory pathways for seabirds. ## Significance Sea level rise is a **linchpin of climate change impacts**, linking atmospheric warming to tangible, often irreversible changes in human and natural systems. Coastal cities—think **New York, Shanghai, Lagos, and Miami**—face heightened flood risk, threatening billions of people and trillions of dollars in assets. For biodiversity, rising seas erode critical habitats, push species toward extinction, and disrupt the provisioning of ecosystem services such as storm protection and carbon sequestration. Understanding the mechanisms behind SLR informs **mitigation** (reducing greenhouse‑gas emissions) and **adaptation** (building sea walls, restoring wetlands, managed retreat). Moreover, sea level data serve as a **global climate indicator**, helping scientists validate climate models and track the effectiveness of international climate agreements. The urgency of addressing sea level rise underscores the broader need for **integrated, science‑based policy** that safeguards both human communities and the planet’s coastal ecosystems. **INFOBOX:** - Name: **Global Mean Sea Level Rise** - Type: **Climate‑change indicator / Oceanographic phenomenon** - Date: **Ongoing; accelerated since the 1970s** - Location: **World‑wide oceans, with regional variations** - Known For: **Fastest sustained rise in the past 3 000 years, driven primarily by anthropogenic warming** **TAGS:** sea level rise, climate change, thermal expansion, glacial melt, coastal erosion, oceanography, climate adaptation, environmental impact
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