Higher metabolic and survival costs induced by predation risk were only partially offset by changes in consumption rates and assimilation efficiencies and the magnitude of non-consumptive effects
varied as a function of temperature.
Not exact matches
You have correctly noted that the absolute surface
temperature varies enormously on very short distances
as a
function of the terrain (something that is true for rural
as well
as urban environments).
Functions such
as hormonal secretions, heart rate, body
temperature and feelings
of sleepiness and alertness
vary regularly with peaks and troughs across the day.
The exact way that intensities and fluxes
vary as a
function of CSD depends on the spatial
temperature distribution
as well
as the Planck
function, or in combination, it depends on the spatial distribution
of the Planck
function (for local
temperature).
Trends
as a
function of CSD, Saturation: If the
temperature varies monotonically over the distance from which most
of the radiation reaching that level is emitted, then increasing the CSD will bring the upward and downward fluxes and intensities (at a given angle) toward the same value, reducing the net intensities and fluxes, until eventually they approach zero (or a nonzero saturation value at TOA).
Including emission along a path (Schwarzchild's equation), a flux will approach saturation
as the optical thickness becomes large over scales where the
temperature variation is small; at smaller optical thicknesses, the
temperature distribution may
vary and larger
temperature variations make the nonlinearity
of the Planck
function important, but over short distances, the
temperature variation can be approximated
as linear and the associated Planck
function values can be approximated
as linearly proportional to distance for small
temperature changes, so the flux will approach an asymptotic value
as a hyperbolic
function (the difference between the flux and the saturation value
of the flux will be proportional to 1 / optical thickness per unit distance (assuming isotropic optical properties (or even somewhat anisotropic properties), it will have that proportionality for all directions and thus for the whole flux across an area).
Thus there is convection within the troposphere that (to a first approximation) tends to sustain some lapse rate profile within the layer — that itself can
vary as a
function of climate (and height, location, time), but given any relative
temperature distribution within the layer (including horizontal and temporal variations and relationship to variable CSD contributors (water vapor, clouds)-RRB-, the
temperature of the whole layer must shift to balance radiative fluxes into and out
of the layer (in the global time averae, and in the approximation
of zero global time average convection above the troposphere), producing a PRt2 (in the global time average) equal to RFt2.
Water Use per Acre
of Almonds: All crops require water and the total water requirement
varies throughout the growing season
as a
function of temperature and other climatic factors, the characteristics
of the plants themselves, soil conditions, irrigation methods and efficiencies, and more.
Because IR in these wavelengths is not efficiently intercepted by greenhouse gases, its intensity
varies mainly
as a
function of surface
temperature, according to the Stefan - Boltzmann law.
It is however, not considered
as a climate «forcing» because the amount
of H2O in the air
varies basically
as a
function of temperature.»
Soil
temperature varies from month to month
as a
function of incident solar radiation, rainfall, seasonal swings in overlying air
temperature, local vegetation cover, type
of soil, and depth in the earth.
If I was really obsessive about this I could mount the IR thermometer on a jig where I could precisely
vary the angle and measure the
temperature as a
function of angle.