Although climate variations and sea level changes are often discussed interchangeably, climate change need not always result in sea level change. Perturbations in Earth's orbit cause major climate changes, and the resulting variations in the amount and distribution of solar radiation at ground level follow cycles lasting for thousands of years. Research done in the last decade shows that climate can change on centennial or shorter time scales. These more rapid changes appear to be related to modifications in ocean circulation initiated during the last glacial period either by injections of fresh meltwater or huge ice discharges into the North Atlantic. When first detected, these rapid climate changes were characterized as episodes decoupled...
On 103- to 106-year timescales, global sea level is determined largely by the volume of ice stored o...
During glacial periods of the Late Pleistocene, an abundance of proxy data demonstrates the existenc...
It is likely that the anticipated warming due to the effect of increasing concentration of carbon d...
The oscillations between glacial and interglacial climate conditions over the past three million yea...
Sea level variations have been, are, and will always be taking place on local, regional, and global ...
Earths climate has oscillated between short-lived interglacial and extended glacial periods for the ...
Understanding how and why global climate is changing is investigated at the astronomical time scale ...
The geologic record provides constraints on the rates, amplitudes, and mechanisms controlling global...
Following the Last Glacial Maximum (25,000–20,000 years ago), sea level rose at rates on the order o...
International audienceWe review present‐day observations of sea level change and variability at glob...
Following the Last Glacial Maximum (25,000–20,000 years ago), sea level rose at rates on the order o...
Climate states of warm and cold periods have varied on approximately 100,000 year cycles for the las...
Climate states of warm and cold periods have varied on approximately 100,000 year cycles for the las...
Climate states of warm and cold periods have varied on approximately 100,000 year cycles for the las...
The Earth\u27s climate has undergone a global transition over the past four million years, from warm...
On 103- to 106-year timescales, global sea level is determined largely by the volume of ice stored o...
During glacial periods of the Late Pleistocene, an abundance of proxy data demonstrates the existenc...
It is likely that the anticipated warming due to the effect of increasing concentration of carbon d...
The oscillations between glacial and interglacial climate conditions over the past three million yea...
Sea level variations have been, are, and will always be taking place on local, regional, and global ...
Earths climate has oscillated between short-lived interglacial and extended glacial periods for the ...
Understanding how and why global climate is changing is investigated at the astronomical time scale ...
The geologic record provides constraints on the rates, amplitudes, and mechanisms controlling global...
Following the Last Glacial Maximum (25,000–20,000 years ago), sea level rose at rates on the order o...
International audienceWe review present‐day observations of sea level change and variability at glob...
Following the Last Glacial Maximum (25,000–20,000 years ago), sea level rose at rates on the order o...
Climate states of warm and cold periods have varied on approximately 100,000 year cycles for the las...
Climate states of warm and cold periods have varied on approximately 100,000 year cycles for the las...
Climate states of warm and cold periods have varied on approximately 100,000 year cycles for the las...
The Earth\u27s climate has undergone a global transition over the past four million years, from warm...
On 103- to 106-year timescales, global sea level is determined largely by the volume of ice stored o...
During glacial periods of the Late Pleistocene, an abundance of proxy data demonstrates the existenc...
It is likely that the anticipated warming due to the effect of increasing concentration of carbon d...