But the interpretation of the oxygen isotope records is complicated because both isotope storage in ice sheets and deep-water temperature affect the recorded isotopic composition. Separating these two effects would require long records of either sea level or deep-ocean temperature, which are currently ...
Assertion : At high altitudes liquids boil at lower temperaturers in comparison to that of sea level. Reason : At high altitudes atmospheric pressure is low ABoth assertion and reason are true and reason is the correct explanation of assertion BBoth assertion and reason are true and reason ...
“Tiny changes in the radio signal can be measured by the instrument, which relate to the density of the atmosphere,” added Ao. “We can then precisely determine the temperature, pressure, and humidity through the layers of the atmosphere, which give us incredible insights t...
The terminus position,L, is a direct output of the simulations while the cumulative sea level contribution per unit width of glacier in yeart, SLR, is calculated as\(\,{{\mbox{SLR}}}\,=\int\nolimits_{1979}^{t}\left(PL-Q\right)\,{\mathrm{d}}{t}^{\prime}\). In order to fac...
52 The emphasis that these two expressions refer to the absorption coefficients at a reference temperature of 296 K is missing in eqs. (12) and (13) of Ref. 50. It should also be noted that in the notation of Ramanathan and Downey,50 the k1vand k2vgiven here are referred to as K2...
where H was computed from temperature data as the lowest pressure level at which the lapse rate decreases to 2 °C/km [337], ΔH is the tropospheric mean meridional potential temperature gradient, and Ω is the angular velocity of the earth. From the thermodynamic equation and the mass conti...
Atmosphere–ocean interactions are known to dominate seasonal to decadal sea level variability in the southeastern North Sea. In this study an atmospheric proxy for the observed sea level variability in the German Bight is introduced. Monthly mean sea level (MSL) time series from 13 tide gauges ...
Rasmussen, E. M. and T. H. Carpenter, 1982: ‘Variations in tropical sea surface temperature and surface wind fields associated with the Southern 0scillation/El Nino’.Monthly Weather Review,110, 354–384. ArticleGoogle Scholar Reiter, E. R., 1972:Atmospheric Transport Processes, Part 3: Hy...
This is due to anomalous horizontal transport and convergence of sensible heat and moisture in the lower atmosphere, which increases both downward sensible heat flux and downwelling long-wave radiation at the surface. On an hourly timescale, over 70% of extreme warm-temperature anomalies occur ...
Correlations are considered significant at the 95% level when they exceed one standard error.Data availability NOAA 1/4° daily Optimum Interpolation Sea Surface Temperature (OISST) are available from https://www.ncdc.noaa.gov/oisst. NCEP daily reanalyses of atmospheric pressure, heat fluxes and ...