Not exact matches
The
observed increase in freshwater content will affect the
conditions in all Greenland fjords and may ultimately affect the global
ocean currents that keep Europe warm.
While acidic
conditions are known to dissolve calcium carbonate, the method of skeleton construction that Gilbert
observed in this study should be much more stable in the face of acidifying
oceans.
Using
observed and modeled
ocean current
conditions, they found a difference of distance between the turtles and drifters to be as much as 125 miles in the first few days.
Ed Miles, a professor of marine studies and public affairs at the University of Washington, said the prospect of a coordinated federal
ocean acidification research program is welcome news, especially given the
conditions Feely
observed off the California coast in 2008.
NASA's Earth -
observing satellites help monitor those and other impacts by measuring land and
ocean conditions that both influence and are affected by El Niño.
The accessibility of a large numbers of tidewater glaciers, subject to warming
conditions, provides a unique opportunity to
observe processes and enable more accurate predictions of sea level response to
ocean warming around Antarctica.
This novel approach finds local populations in the North Pacific and Northwest Atlantic are regionally synchronized and strongly correlated to
ocean conditions — such that climate models alone explain up to 88 % of the
observed changes over the past several decades.
Since it has been so long since the last nesting was
observed here, scientists surmised that recent
ocean conditions could be the reason for the re-establishment of this seabird colony.
«Dr Jim Maslanek of the University of Colorado, Boulder to
observe the «Spatial and Temporal Variability of
Ocean and Ice
Conditions In and Near the Marginal Ice Zone»
Ensemble simulations conducted with EMICs (Renssen et al., 2002; Bauer et al., 2004) and coupled
ocean - atmosphere GCMs (Alley and Agustsdottir, 2005; LeGrande et al., 2006) with different boundary
conditions and freshwater forcings show that climate models are capable of simulating the broad features of the
observed 8.2 ka event (including shifts in the ITCZ).
«Using a GCM, can we regenerate the land temperature record from the
ocean record using
observed SSTs and sea ice distribution as a boundary
condition?
Here a simple biologically and physically - based model of sapflow potential is used to assess
observed changes in sapflow across the Northeastern US from 1980 to 2006; document the correspondence between these observations and independent downscaled atmosphere
ocean general circulation model (AOGCM) simulations of
conditions during this period; and quantify changes in sapflow potential through 2100.
Simulation of cumulus clouds under
conditions observed during the Rain in Cumulus over the
Ocean (RICO) field campaign.
Across the
oceans, record warmth was
observed scattered across all
oceans, while cooler - than - average
conditions were limited to the North Atlantic
Ocean, central and eastern tropical as well as southeastern Pacific
Ocean, and across parts of the eastern Indian
Ocean.
As with previous CIS contributions, the 2016 forecast was derived by considering a combination of methods: 1) a qualitative heuristic method based on
observed end - of - winter Arctic ice thickness / extent, as well as winter surface air temperature, spring ice
conditions and the summer temperature forecast; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent time - series into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests
ocean, atmosphere and sea ice predictors.
Importantly, the MEI does not distinguish between natural and anthropogenic changes in climate forcing, but instead provides an integrated index of climate
conditions for comparison with
observed changes in
ocean productivity.»
Background mixing in the deep
ocean is related to internal wave energy, which in ice - covered seas has been
observed to be lower than in ice - free
oceans, and to change with time and bathymetric
conditions [Levine et al., 1985 and 1987; Halle and Pinkel, 2003; Pinkel, 2005].
The
observed pattern of
ocean temperature change created a propensity for drought in some regions around the globe — perhaps including California, which has been experiencing drought
conditions more often than not over the past decade and a half.
To answer this question, large ensemble simulations of regional climate models will be carried out for an East Asian domain for two worlds: (1) Real world
condition for which the
observed sea surface temperatures will be prescribed and (2) Counter-factual world
condition for which we will use adjusted sea surface temperatures obtained by removing human - induced
ocean warming patterns.