Sentences with phrase «ocean observations from»

In the meantime, Keenlyside and colleagues plan to incorporate the increased ocean observations from the last 10 years into their forecast system.
As Stephen C. Riser and M. Susan Lozier note in their February 2013 Scientific American article, «Rethinking the Gulf Stream,» «A comparison of the Argo data with ocean observations from the 1980s, carried out by Dean Roemmich and John Gilson of the Scripps Institution of Oceanography, shows that the upper few hundred meters of the oceans have warmed by about 0.2 degree C in the past 20 years.

Not exact matches

Suspicions that Saturn's icy moon Enceladus harbors an internal ocean — one that could host life — have hardened into near certainty with exquisitely precise observations from the Cassini spacecraft.
Observations show that the Southern Ocean is still pulling CO2 from the sky, but that may not last forever
Given that ocean observations for climate provide a wide range of benefits to the agricultural, shipping, fishing, insurance, and energy - supply industries, the committee that wrote the report suggested that efforts could be made to draw support for ocean observing from the commercial sector.
This global biological recordbased on daily observations of ocean algae and land plants from NASAs Sea - viewing Wide Field - of - View Sensor (SeaWiFS) missionwill enable scientists to study the fate of atmospheric carbon, terrestrial plant productivity and the health of the oceans food web.
Their observations show that since the calving event, the berg has started to drift away from the Larsen - C, with open ocean clearly visible in the ~ 5 kilometre gap between the berg and the ice - shelf.
We present observations of the structure and composition of the shallow source fault of the 2011 Tohoku - Oki earthquake and tsunami from boreholes drilled by the Integrated Ocean Drilling Program Expedition 343 and 343T.
A research group comprising Project Researcher Yusuke Yamashita, Assistant Professor Tomoaki Yamada, Professor Masanao Shinohara and Professor Kazushige Obara at the University of Tokyo Earthquake Research Institute and researchers at Kyushu University, Kagoshima University, Nagasaki University, and the National Research Institute for Earth Science and Disaster Prevention, carried out ocean bottom seismological observation using 12 ocean bottom seismometers installed on the seafloor of Hyuga - nada from April to July 2013.
In June 2006, Chairwoman Mikulski received the Joint Ocean Commission Initiative's (JOCI) report, «From Sea to Shining Sea: Priorities for Ocean Policy Reform,» which recommended robust funding for ocean research, education, observation and exploraOcean Commission Initiative's (JOCI) report, «From Sea to Shining Sea: Priorities for Ocean Policy Reform,» which recommended robust funding for ocean research, education, observation and exploraOcean Policy Reform,» which recommended robust funding for ocean research, education, observation and exploraocean research, education, observation and exploration.
«Hydrothermal siphon» drives water circulation through seafloor: New study explains previous observations of ocean water flowing through the seafloor from one seamount to another.»
By using long - term observations, scientists from the GEOMAR Helmholtz Centre for Ocean Research Kiel have now shown that freshwater has already impacted convection in the last decade.
«If this conclusion is confirmed by future observations, it would mean that the coastal ocean will become more and more efficient at removing carbon dioxide from the atmosphere,» said Goulven Lurallue, the paper's lead author and a researcher with Université Libre de Bruxelles in Belgium.
Satellite observations from GPM, like its satellite predecessor the Tropical Rainfall Measuring Mission, are vital because they can measure rain accumulation over oceans, where the majority of rainfall occurs.
The authors point out that the findings support previous observations of individual male whales moving between populations in different ocean basins, and that subpopulations from both regions could share the same feeding ground in Antarctic waters.
Images from NASA's Galileo probe a few years ago, coupled with previous observations, suggest that Europa's ice - covered surface may conceal a global, liquid ocean tens of kilometers deep.
Co-author Dr Ivan Haigh, lecturer in coastal oceanography at the University of Southampton and also based at NOCS, adds: «Historical observations show a rising sea level from about 1800 as sea water warmed up and melt water from glaciers and ice fields flowed into the oceans.
KAMUELA, HI — Observations of Europa from the W. M. Keck Observatory help NASA and California Institute of Technology (Caltech) astronomers go one step further in demonstrating life may be possible in the ocean of one of Jupiter's moons.
Model results and observations both indicate warming of the world ocean from 1955 to 2003.
The most recent observations of sea surface temperatures across the tropical Pacific Ocean (top) and how different those temperatures are from normal (bottom).
From 1966 to 2003 the modeled mean world ocean temperature in the upper 700 m increased 0.097 Â °C and by 0.137 Â °C according to observations (Levitus et al., 2005); the modeled mean temperature adjusted for sea ice in the corresponding layer of the Arctic Ocean increased 0.203 ocean temperature in the upper 700 m increased 0.097 Â °C and by 0.137 Â °C according to observations (Levitus et al., 2005); the modeled mean temperature adjusted for sea ice in the corresponding layer of the Arctic Ocean increased 0.203 Ocean increased 0.203 Â °C.
The OceanObs»09 conference (Venice, Italy) involved more than 600 participants from 36 countries who defined a vision for societally beneficial ocean observations to be sustained over the next decade.
The historical observations from Hadley Centre & Simple Ocean Data Assimilation (SODA) datasets are at the bottom.
Field observations of microbes recovered from deep drill cores, deep mines, and the ocean floor, coupled with laboratory investigations, reveal that microbial life can exist at conditions of extreme temperatures (to above 110ºC) and pressures (to > 10,000 atmospheres) previous thought impossible.
To get their results the researchers used sophisticated ice sheet and climate models and verified their results with independent geological observations from the oceans off Antarctica.
By combining the ocean heating rates, TOA observations (figure 4) and other energy storage terms (land, atmosphere warming and ice melt), the authors calculated Earth's energy imbalance from January 2001 - December 2010 to be 0.5 (± 0.43) W / m2.
Rather than use a model - based estimate, as did Hansen (2005) and Trenberth (2009), the authors achieve this by calculating it from observations of ocean heat content (down to 1800 metres) from the PMEL / JPL / JIMAR data sets over the period July 2005 to June 2010 - a time period dominated by the superior ARGO - based system.
a, Global annual average (July to June) net TOA flux from CERES observations and 0 — 700 and 0 — 1,800 m ocean heating rates from PMEL / JPL / JIMAR.
The decrease over the last 20 years is well substantiated by observation and is indistinguishable from the calculated decline assuming that the surface ocean is in near thermodynamic equilibrium with increasing CO2 concentration of the atmosphere.
However, comparison of the global, annual mean time series of near - surface temperature (approximately 0 to 5 m depth) from this analysis and the corresponding SST series based on a subset of the International Comprehensive Ocean - Atmosphere Data Set (ICOADS) database (approximately 134 million SST observations; Smith and Reynolds, 2003 and additional data) shows a high correlation (r = 0.96) for the period 1955 to 2005.
Norris, J.R., 1998a: Low cloud type over the ocean from surface observations.
Based on model experiments, it has been suggested that errors resulting from the highly inhomogeneous distribution of ocean observations in space and time (see Appendix 5.
The figure below, taken from the 2007 IPCC report, shows model runs with only natural forcings; model runs with all forcings; and observations of surface temperatures for the whole globe — land areas and ocean areas.
The fact that the observations have a «memory» from month to month (because the ocean is slow to change temperature) allows us to predict the annual mean from the year - to - date average (which implicitly includes the ENSO effect).
A large ensemble of Earth system model simulations, constrained by geological and historical observations of past climate change, demonstrates our self ‐ adjusting mitigation approach for a range of climate stabilization targets ranging from 1.5 to 4.5 °C, and generates AMP scenarios up to year 2300 for surface warming, carbon emissions, atmospheric CO2, global mean sea level, and surface ocean acidification.
The Fourth Assessment Report finds that «Warming of the climate system is unequivocal, as is now evident from observations of increases in global average air and ocean temperatures, widespread melting of snow and ice, and rising mean sea level.
From its base in Namibia, the Observations of Clouds above Aerosols and their Interactions (ORACLES) study will use airborne instruments this fall to probe the impact on climate and rainfall of the interaction between clouds over the southeastern Atlantic Ocean and smoke from vegetation burning in southern AfrFrom its base in Namibia, the Observations of Clouds above Aerosols and their Interactions (ORACLES) study will use airborne instruments this fall to probe the impact on climate and rainfall of the interaction between clouds over the southeastern Atlantic Ocean and smoke from vegetation burning in southern Afrfrom vegetation burning in southern Africa.
Made from fibreglass, steel and concrete, the Bathurst Pineapple is complete with a gift shop, tourist information centre and observation deck, boasting views that stretch as far as the Indian Ocean.
It has a great floor plan, Spectacular Ocean and Reef views from the observation deck and the large veranda.
Yonder observation across the blue ocean from Nusa Lembongan Island will relentlessly captivate your much admiration.
, and expansive ocean and sound views from its elevated observation deck.
And since we don't have good ocean heat content data, nor any satellite observations, or any measurements of stratospheric temperatures to help distinguish potential errors in the forcing from internal variability, it is inevitable that there will be more uncertainty in the attribution for that period than for more recently.
Field observations from the Beaufort Sea to Hudson Bay are suggesting that the food web in the Arctic Ocean is ailing, causing many species to flounder as a result of the warming environment.
«GSSL, GOHC and GOFC derived from in situ observations are a useful benchmark for ocean and climate models and an important diagnostic for changes in the Earth's climate system (Hansen et al., 2005; Levitus et al., 2005).
In these experiments the climate sensitivity was 2.7 deg C for a doubling of CO2, the net aerosol forcing from 1940 to 2000 was around -0.7 W / m2 (55 % of the total forcing, -1.27, from 1850 to 2000), and the ocean uptake of heat was well - matched to recent observations.
The model variables that are evaluated against all sorts of observations and measurements range from solar radiation and precipitation rates, air and sea surface temperatures, cloud properties and distributions, winds, river runoff, ocean currents, ice cover, albedos, even the maximum soil depth reached by plant roots (seriously!).
Model results and observations both indicate warming of the world ocean from 1955 to 2003.
Hatun et al. also used altimeter data (local sea level height measurements from satellite observations) to diagnose the norther oceans gyre circulation.
Summary for Policymakers Chapter 1: Introduction Chapter 2: Observations: Atmosphere and Surface Chapter 3: Observations: Ocean Chapter 4: Observations: Cryosphere Chapter 5: Information from Paleoclimate Archives Chapter 6: Carbon and Other Biogeochemical Cycles Chapter 7: Clouds and Aerosols Chapter 8: Anthropogenic and Natural Radiative Forcing Chapter 8 Supplement Chapter 9: Evaluation of Climate Models Chapter 10: Detection and Attribution of Climate Change: from Global to Regional Chapter 11: Near - term Climate Change: Projections and Predictability Chapter 12: Long - term Climate Change: Projections, Commitments and Irreversibility Chapter 13: Sea Level Change Chapter 14: Climate Phenomena and their Relevance for Future Regional Climate Change Chapter 14 Supplement Technical Summary
From 1966 to 2003 the modeled mean world ocean temperature in the upper 700 m increased 0.097 Â °C and by 0.137 Â °C according to observations (Levitus et al., 2005); the modeled mean temperature adjusted for sea ice in the corresponding layer of the Arctic Ocean increased 0.203 ocean temperature in the upper 700 m increased 0.097 Â °C and by 0.137 Â °C according to observations (Levitus et al., 2005); the modeled mean temperature adjusted for sea ice in the corresponding layer of the Arctic Ocean increased 0.203 Ocean increased 0.203 Â °C.
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