According to the researchers, to better understand if Matthew's intensification was aided by the warm - water eddies and the residing barrier layer in the Caribbean Sea's upper ocean, more ambient and in - storm
upper ocean observations in this basin are needed to improve forecast models for the region.
Not exact matches
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.
The collection of larger than usual amounts of Arctic winter weather data in 2015 was due to two reasons: the Norwegian research vessel Lance was in the Arctic
Ocean observing and collecting
upper atmosphere meteorological data, and the frequency of
observation and data collection was increased at some of the land - based
observation stations around the Arctic.
Observations of
upper ocean heat show some short term cooling but measurements to greater depths (down to 2000 metres) show a steady warming trend: However, the
ocean cooling myth does seem to be widespread so I'll shortly update this page to clarify the issue.
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.
Study of
upper ocean dynamics and air - sea interaction; investigation of the
ocean's role in climate; sustained climate - quality
observations in and at the surface of the
ocean; innovative
ocean observations.
OBSERVATION DECKS The
upper decks are generally open for viewing wildlife and enjoying the open
ocean.
Our whale watching tour allows Long Beach visitors and residents to enjoy a relaxing cruise on The
Ocean Explorer, our primary whale watching cruise ship, complete with both indoor and outdoor seating and a
upper level
observation deck.
It seems to me that they must show deeper mixing than 50 M, since there is not enough mass in the
upper 50 meters of
ocean to account for the annual heat storage changes that are implied by
observations for the the full integrated 700 meter volume of
ocean.
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.
This is supported by historic
observations (Figure 1), which shows roughly decade - long hiatus periods in
upper ocean heat content during the 1960s to 1970s, and the 1980s to 1990s.
Forest et al. 2006 compares
observations of multiple surface,
upper air and deep -
ocean temperature changes with simulations thereof by the MIT 2D climate model run at many climate parameter settings.
That leads to the IPCC conclusion that it is «very likely» that anthropogenic factors have «made a substantial contribution to
upper ocean warming» using a method independent of
observation estimates of the value of individual fluxes.
There are three likelihood functions involved, one for each of the three «diagnostics» — surface,
upper - air, and deep -
ocean, which involve respectively 20, 218 and 1
observation (s).
In many cases, the lack or insufficient quality of long - term
observations, be it a specific variable, an important processes, or a particular region (e.g., polar areas, the
upper troposphere / lower stratosphere (UTLS), and the deep
ocean), remains an impediment.
But the NASA researchers said their approach, described in the journal Nature Climate Change, is the first to test the idea using satellite
observations, as well as direct temperature measurements of the
upper ocean.
An updated analysis by Durack and colleagues found that from 1970 to 2004, the
upper 700 meters of
oceans in the Southern Hemisphere had gained from 48 to 166 percent more heat than estimated from earlier
observations.
These
observations improve the forecasts of currents in the
upper ocean.
- At NERSC we use these satellite
observations for research and development studies of the
upper ocean and sea ice covered regions, with special focus in the Nordic Seas and Arctic O
ocean and sea ice covered regions, with special focus in the Nordic Seas and Arctic
OceanOcean.
For these reasons, Section 5.2 mainly assessed
upper -
ocean observations for long - term trends in heat content and salinity.
Several studies have shown that
observations of sea surface height (SSH) are strongly correlated with the thermal structure of the
upper ocean (e.g. Goni et al. 1996; Gilson et al. 1998; Mayer et al. 2001; Willis et al. 2004).
«In many cases, the lack of long term
observations,
observations suitable for the evaluation of important processes, or
observations in particular regions (e.g., polar areas, the
upper troposphere / lower stratosphere (UTLS), and the deep
ocean) remains an impediment.»
Develop and validate retrieval algorithms for
ocean and sea ice parameters from various satellite Earth
observation data, which in are used in studies of
upper layer mesoscale
ocean processes, air - sea - ice interaction, climate change studies and in operational oceanography.
Observations suggest lower values for climate sensitivity whether we study long - term humidity,
upper tropospheric temperature trends, outgoing long wave radiation, cloud cover changes, or the changes in the heat content of the vast
oceans.
Observations showing that the skin (top tens of um) of the
ocean is usually colder than the water below convincing demonstrate that increasing DLR will warm the
upper ocean and that Hypothesis A and B are untenable.
Satellite
observations provide near - global coverage and thus represent an important source of information over the
oceans, where radiosonde
observations are scarce, and in the
upper troposphere, where radiosonde sensors are often unreliable.
By warming the
upper ocean (agrees with
observations) and reducing low cloud cover (unclear from
observations: ISCCP data are routinely over - interpreted / downright misrepresented on this point).
«Whilst the last decade has seen a rapid increase in good
observations of the surface and
upper ocean, thanks to Argo floats, we have very few for the deep
ocean.»