Sentences with phrase «regional coastal sea level»

New research published this week in the Journal of Climate reveals that one key measurement — large - scale upper - ocean temperature changes caused by natural cycles of the ocean — is a good indicator of regional coastal sea level changes on these decadal timescales.

Not exact matches

The report, «Global and Regional Sea Level Rise Scenarios for the United States,» provides regional sea - level rise scenarios and tools for coastal preparedness planning and risk managemeSea Level Rise Scenarios for the United States,» provides regional sea - level rise scenarios and tools for coastal preparedness planning and risk manageLevel Rise Scenarios for the United States,» provides regional sea - level rise scenarios and tools for coastal preparedness planning and risk managemesea - level rise scenarios and tools for coastal preparedness planning and risk managelevel rise scenarios and tools for coastal preparedness planning and risk management.

Sea level rise is a significant threat to the world's coastal areas, but the threat is not the same everywhere on Earth — it depends on many regional factors.

Rising sea levels will make coastal areas more prone to flooding, regional droughts are likely to increase in frequency and intensity, summer months are likely to have more extreme - heat days, and thunderstorms and other weather events are likely to become more intense in some parts of the world.

The overarching goal of this WCRP research effort, led by WCRP's Core Project «Climate and Ocean Variability, Predictability and Change» (CLIVAR) as a Research Focus, is to establish a quantitative understanding of the natural and anthropogenic mechanisms of regional to local sea level variability; to promote advances in observing systems required for an integrated sea level monitoring; and to foster the development of sea level predictions and projections that are of increasing benefit for coastal zone management.

By the late 21st century, climate models project that sea level will rise up to a foot higher than the global average along the northeast US coastline, resulting in a dramatic increase in regional coastal flood risk.

Lukovich et al. (Centre for Earth Observation Science, U. of Manitoba); 4.6; Heuristic - Dynamics Investigation of dynamical atmospheric contributions in spring to sea ice conditions in fall, based on comparison of 2011 and 2007 stratospheric and surface winds and sea level pressure (SLP) in April and May suggests regional differences in sea ice extent in fall, in a manner consistent with recent studies highlighting the importance of coastal geometry in seasonal interpretations of sea ice cover (Eisenman, 2010).

In the future, high - end estimates of ice discharge and regional effects, such as local thermal expansion and coastal subsidence, place the upper limits of relative sea - level rise for the Netherlands at 0.65 to 1.3 m by 2100, excluding gravitational effects.

Analyses of tide gauge and altimetry data by Vinogradov and Ponte (2011), which indicated the presence of considerably small spatial scale variability in annual mean sea level over many coastal regions, are an important factor for understanding the uncertainties in regional sea - level simulations and projections at sub-decadal time scales in coarse - resolution climate models that are also discussed in Chapter 13.

Mean sea level (MSL) evolution has a direct impact on coastal areas and is a crucial index of climate change since it reflects both the amount of heat added in the ocean and the mass loss due to land ice melt (e.g. IPCC, 2013; Dieng et al., 2017) Long - term and inter-annual variations of the sea level are observed at global and regional scales.

Renewable energy cooperation will also promote economies of scale and fraternal ties crucial to dealing with the other pressing climate impacts faced by many regional states: growing water scarcity amid shifting weather patterns and, in some, projected sea - level rises on coastal communities and aquifers.

A recent study on the North Pacific circulation patterns over the past 1.2 million years determined that sea ice on coastal areas can be an important factor in ocean circulation, therefore influencing climate at global and regional levels.