The surface heat flux response to underlying sea surface temperature (SST) anomalies (the surface heat flux feedback) is estimated using 42 yr (1956–97) of ship-derived monthly turbulent heat fluxes and 17 yr (1984–2000) of satellite-derived monthly radiative fluxes over the global oceans for individual seasons. Net surface heat flux feedback is generally negative (i.e., a damping of the underl...

[1] This paper synthesizes a variety of atmospheric and oceanic data to examine the large-scale energy budget of the Arctic. Assessment of the atmospheric budget relies primarily on the ERA-40 reanalysis. The seasonal cycles of vertically integrated atmospheric energy storage and the convergence of energy transport from ERA-40, as evaluated for the polar cap (defined by the 70 N latitude circle...

ANDREOLI, THOMAS E., JAMES A. SCHAFER, SUSAN L. TROUTMAN, AND MARY L. WATKINS. Solvent drag component of Clflux in superficial proximal straight tubules: evidence for a paracellular component of isotonic fluid absorption. Am. J. Physiol. 237(6): F455-F462, 1979 or Am. J. Physiol.: Renal Fluid Electrolyte Physiol. 6(6): F455-F462, 1979.-We have computed the fraction of isotonic fluid absorption ...

In response to osmotic perturbation, the Amphiuma red blood cell regulates volume back to "normal" levels. After osmotic swelling, the cells lose K, Cl, and osmotically obliged H2O (regulatory volume decrease [RVD] ). After osmotic shrinkage, cell volume is regulated as a result of Na, Cl, and H2O uptake (regulatory volume increase [RVI] ). As previously shown (Cala, 1980 alpha), ion fluxes res...

The freshwater flux from the Greenland Ice Sheet (GrIS) to the ocean is of considerable importance to the global eustatic sea level rise. A physical modelling approach using SnowModel, a state-of-the-art snow-evolution modelling system that includes four submodels (MicroMet, EnBal, SnowPack, and SnowTran-3D), was used to quantify the 1995–2007 GrIS surface massbalance (SMB), including freshwate...

We have explored intestinal function in the euryhaline killifish Fundulus heteroclitus after transfer from brackish water (10% seawater) to fresh water. Plasma Na+ and Cl- concentrations fell at 12 h post-transfer, but recovered by 7 days. Drinking rate decreased substantially at 12 h (32% of control value) and remained suppressed after 3 and 7 days in fresh water (34 and 43%). By contrast, the...

Fluxes of both acidic equivalents (JH+net) and electrolytes across the gills were continuously monitored in the freshwater rainbow trout (Salmo gairdneri) during 24 h normoxia (PIO2 = 120-150 torr; control), 72 h hyperoxia (PIO2 = 500-600 torr), and 24 h return to normoxia. A highly negative JH+net (i.e., excretion) was responsible for over 90% of the compensation of respiratory acidosis induce...

We present Mars Atmosphere and Volatile EvolutioN (MAVEN) observations of Marsward and tailward fluxes of suprathermal (>25 eV) ions in the near-Mars (∼1–1.5 Mars radii downstream) magnetotail. Statistical results show that the Marsward proton flux and magnetic field draping pattern are well organized by the upstream motional electric field direction. We observe both significant Marsward proton...