Extreme sea level rise along the Indian Ocean coastline: observations and 21st century projections

نویسندگان

چکیده

Abstract Anthropogenic sea-level rise poses challenges to coastal areas globally. The combined influence of rising mean sea level (MSL) and storm surges exacerbate the extreme (ESL). Increasing ESL a major challenge for climate change adaptation nearly 2.6 billion inhabitants in Indian Ocean region. Yet, knowledge about past occurrences its progression is limited. Combining multiple tide-gauge satellite-derived data, we show that has become more frequent, longer-lasting intense along coastlines. We detect 2–3-fold increase occurrence, with higher risk Arabian Sea coastline Islands. Our results reveal MSL primary contributor (more than 75%), additional contribution from intensifying tropical cyclones. A two-fold detected an 0.5 °C warming relative pre-industrial levels. Utilizing likely range (17th–83rd percentile as spread) Intergovernmental Panel on Climate Change projections considerable inter-model spread, region will be exposed annually present-day 100 year event by 2100, irrespective greenhouse-gas emission pathways, 2050 under moderate-emission-mitigation-policy scenario. study provides robust regional estimate MSL, which important policies.

برای دانلود باید عضویت طلایی داشته باشید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Ocean Currents Modeling along the Iranian Coastline of the Oman Sea and the Northern Indian Ocean

The Makran Coast (Iranian Coastline of the Oman Sea on the Northern Indian Ocean) plays an important role in country’s future navigation and trade due to its accessibility. In 2014, the Iranian Makran coastline was selected by the PMO to be studied as the Phase 6 in the series of Monitoring and Modelling Studies of Iranian Coasts with all disciplines being in investigated including currents. Al...

متن کامل

Efficacy of geoengineering to limit 21st century sea-level rise.

Geoengineering has been proposed as a feasible way of mitigating anthropogenic climate change, especially increasing global temperatures in the 21st century. The two main geoengineering options are limiting incoming solar radiation, or modifying the carbon cycle. Here we examine the impact of five geoengineering approaches on sea level; SO(2) aerosol injection into the stratosphere, mirrors in ...

متن کامل

Sea-level rise at tropical Pacific and Indian Ocean islands

Historical and projected sea-levels for islands in the tropical Pacific and Indian oceans are a subject of considerable interest and some controversy. The large variability (e.g. El Niño) signals and the shortness of many of the individual tide-gauge records contribute to uncertainty of historical rates of sea-level rise. Here, we determine rates of sea-level rise from tide gauges in the region...

متن کامل

A new approach to projecting 21st century sea-level changes and extremes: 21st century sea level

Future increases in flooding potential around the world’s coastlines from extreme sea level events is heavily dependent on projections of future global mean sea level (GMSL) rise. Yet, the two main approaches for projecting 21st century GMSL rise—i.e., process-based versus semi-empirical—give inconsistent results. Here, a novel hybrid approach to GMSL projection, containing a process-based ther...

متن کامل

Sea level rise in the Arctic Ocean

About 60 tide-gauge stations in the Kara, Laptev, East-Siberian and Chukchi Seas have recorded the sea level change from the 1950s through 1990s. Over this 40-year period, most of these stations show a significant sea level rise (SLR). In light of global change, this SLR could be a manifestation of warming in the Arctic coupled with a decrease of sea ice extent, warming of Atlantic waters, chan...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

ژورنال

عنوان ژورنال: Environmental Research Letters

سال: 2022

ISSN: ['1748-9326']

DOI: https://doi.org/10.1088/1748-9326/ac97f5