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Researcher studying the relationship between gene regulation, environment and visible traits. Gibert and collaborators investigated temperature-dependent pigmentation in Drosophila, linking phenotypic plasticity to a network of chromatin regulators.^[ref]

The Jeans escape parameter compares a particle's gravitational binding energy with its thermal energy at a specified atmospheric level. For particle mass $m$, planetary mass $M_p$, radius $r$ and local temperature $T$,Here the second speed uses the factor-two thermal speed convention. For a locally hydrostatic ideal gas, $H=k_{B}T/(mg)$ and $g=G{M}_p/r^2$ also give $\lambda =r/H$; a large parameter is therefore consistent with a thin atmospheric scale height.

In the Maxwellian Jeans escape model at the exobase, the outward Jeans escape flux contains $(1+\lambda )e^{-\lambda }$. Large $\lambda$ suppresses this high-speed tail exponentially, but no finite positive temperature makes it vanish exactly.

A small $\lambda$ warns that a static, thin-atmosphere tail calculation can fail. It does not by itself prove a particular hydrodynamic escape rate: the collision environment, heating and cooling must support the bulk outflow. The parameter uses the upper-atmosphere temperature, which need not equal the planetary equilibrium temperature.

Jelle S. Kaastra develops the physical interpretation of X-ray radiation spectra from hot astronomical plasma. His review with collaborators explains how ionization equilibrium, spectral lines and continuum radiation constrain the diffuse gas in galaxy clusters and between galaxies.

A spectrum acts as a diagnostic because different ions and transitions respond differently to temperature and other physical conditions. The interpretation requires an atomic model: an observed spectral line is evidence about the emitting plasma, rather than a direct reading of a single universal temperature.^[ref]

Jinn-Wen Hwang wrote the 1972 thesis Thermal expansion of nickel and iron, and the influence of nitrogen on the lattice parameter of iron at the Curie temperature by Jinn-Wen Hwang. Its X-ray diffraction measurements connect the lattice parameter of nickel and iron to temperature and the magnetic transition near the Curie temperature. The institutional record identifies it as a master's thesis in metallurgical engineering; no later biography is inferred from that credit.^[ref]

Joan Garcia-Porta is a biologist studying how organisms adapt and diversify in new environments. His research combines phylogenetics, morphology, ecology and genomics, with investigations of lizards, birds and plants. A recurring question is how environmental differences become differences among populations and species.^[ref]

In a 2019 study, Joan Garcia-Porta and collaborators combined phylogenomics and fossil calibration to reconstruct a dated phylogenetic tree of 262 species of Lacertidae. They compared this evolutionary history with occupied climate conditions, preferred body temperature and evaporative water loss. Temperate lineages showed slower molecular substitution rates than tropical and desert-adapted lineages.^[ref]

The illuminating feature is the combination of timescales: DNA differences inform relationships over evolutionary time, while physiological measurements describe what living lizards do now. Their agreement can support a proposed connection between climate and adaptation. A comparative association still needs interpretation; a phylogenetic tree alone does not experimentally demonstrate the cause of a physiological difference.

Joan Wrobel explains the sensitivity of radio interferometers through the relation between source signal and instrumental noise. Her 2004 synthesis-imaging lecture derives the system-equivalent flux density from antenna collecting area, efficiency and system temperature.

The lecture then distinguishes the noise of a single baseline measurement from the sensitivity of a reconstructed image. Tracking those definitions matters when comparing observing proposals or uncertainty estimates: a signal quoted per synthesized beam is not the same quantity as a baseline's flux-density noise.^[ref]

Joel B. Fowler is an electrical engineer whose work at NIST included the design and characterization of a water-bath blackbody source for radiometry. His 1995 paper describes a cavity whose temperature and effective emissivity could be controlled and measured accurately.^[ref]

The apparatus placed a shaped copper cavity in a stirred, temperature-controlled water bath. The cavity geometry increases the number of internal specular reflections, raising its effective emissivity toward one, while the bath reduces temperature variation. The paper reports operation from 278 K to 353 K and calculated emissivity 0.9997, increased to 0.99997 with a restricted aperture. Geometry, thermal control and measurement uncertainty accounting therefore work together to create a useful measurement calibration source.^[ref]

Identity and discipline: upload.wikimedia.org/wikipedia/commons/7/74/A_Third_Generation_Water_Bath_Based_Blackbody_Source_(IA_jresv100n5p591).pdf

John Bertrand Johnson was an electrical engineer whose 1928 measurements established the thermal electrical fluctuations now called Johnson-Nyquist noise. He detected random voltage fluctuations in conductors through a vacuum-tube amplifier and a thermocouple, and related the measured effect to temperature, electrical resistance and the measurement system's frequency response.^[ref]

This reveals why the average voltage alone is not enough to characterize a fluctuating signal. Its expected value can vanish while its mean-square value is positive. The fluctuations become an experimentally measurable noise floor in sensitive electronics, and their temperature dependence connects circuit measurements with the Boltzmann constant.^[ref]

John C. Mather developed and led the scientific use of the COBE FIRAS instrument to test the radiation spectrum of the cosmic microwave background. Comparing the sky signal against a controlled reference blackbody made the measurement a stringent test of spectral shape.

The measured spectrum closely followed Planck's law at a temperature near 2.7 kelvin, strongly supporting a thermal origin in the early Universe. This result addresses a different observable from angular anisotropy: a nearly perfect blackbody spectrum concerns the distribution over frequency, while a sky map concerns changes with direction.^[ref]

John D. Richardson studies space plasmas, including the solar wind and its interaction with the interstellar medium. MIT identifies him as a principal investigator of the Voyager plasma experiment and describes earlier work on plasma transport in planetary magnetospheres.^[ref]

His 2008 Voyager 2 study analyzed plasma measurements across the termination shock. The thermal ions were cooler than a simple picture of bulk-flow energy becoming thermal-ion heat would suggest. The result made the partition of energy among particle populations central to understanding the shock.^[ref]

The experiment illustrates how a remote boundary becomes a local measurement. Four Faraday cups sampled particle currents over energy-per-charge ranges; combining differently oriented detectors allowed the team to infer plasma density, flow and temperature. These inferred properties depend on the measured spectra and distribution model, rather than being direct readings of a thermometer.^[ref]

John Lennard-Jones used gas-transport measurements to constrain models of intermolecular forces. His 1924 work connects the temperature dependence of viscosity with an assumed force law. The familiar modern Lennard-Jones potential represents short-range repulsion and longer-range attraction as $V(r)=4ϵ[(\sigma /r{)}^{12}-(\sigma /r{)}^6]$. Its minimum at $r=2^{1/6}\sigma$ has depth $ϵ$, making the two parameters physically interpretable. This 12–6 form is a simplified interaction model, rather than an exact force law for every atom pair.^[ref]

A physicist associated with the Lennard-Jones potential.

Jonathan Pearce is a metrologist whose research develops practical temperature measurement with contact sensors. His NPL work includes improved thermocouples, models of impurity effects during metal solidification, and methods for detecting or reducing sensor calibration drift. These connect the physics of materials with the reliability of measurements in industrial conditions.^[ref]

In the coauthored Guide on Secondary Thermometry: Industrial Platinum Resistance Thermometers by Jonathan Pearce and others, an important measurement problem is resistance thermometer self-heating: the electrical measuring current heats the sensor whose temperature is being inferred. The guide describes estimating the zero-current resistance from measurements at different currents, while accounting for the surrounding medium. Its treatment of electrical resistance in the leads also explains why four-terminal sensing differs from two-wire measurements. These details show how measurement uncertainty arises from the complete sensor-and-readout arrangement.^[ref]

Homepage: www.npl.co.uk/our-people/jonathan-pearce

Josiah Willard Gibbs was a mathematical scientist whose work gave thermodynamics and statistical mechanics powerful geometric and analytical formulations. His studies of heterogeneous equilibrium connected the behavior of multiple phases and chemical components, while his later work developed a systematic account of statistical ensembles. He also helped establish the practical language of vector calculus.^[ref] His Gibbs free energy combines internal energy, pressure, volume, temperature and entropy as $G=U+pV-TS$. Under the appropriate fixed-temperature and fixed-pressure conditions, its minimization expresses equilibrium, turning a physical stability question into a variational problem.

A long wire with uniform current density $I/(\pi a^2)$ generates uniform heat per volume $H=I^2/({\pi }^2{a}^4\sigma )$. Radial steady conduction obeys $(r{T}_r{)}_r=-Hr/k$. Regularity at the centre removes a logarithmic solution, leaving the displayed parabolic temperature excess relative to the surface. Conductivity, electrical conductivity and current density are assumed constant.

Joule heating is the dissipative conversion of electrical work into internal energy in an electrical conductor. In a metal, the electric field supplies energy to charge carriers, which transfer it to the material. This makes an immersed resistor a useful calibrated heater and makes electrical resistance a source of losses in wiring. Wind-driven electric currents are a proposed source of heating of an inflated giant planet.

For a stationary, purely resistive Ohmic conductor, use the passive sign convention: $V$ is the terminal electric potential difference from the entry to the exit of positive electric current $I$. The absorbed electrical power and Ohm's law giveThe last two expressions assume $V=IR$ at the relevant material temperature. For constant electrical resistance and electric current over a duration $\Delta t$, the dissipated energy is $E_{\mathrm{diss}}=I^{2}R\Delta t$; otherwise use $E_{\mathrm{diss}}=\int V(t)I(t)dt$. In SI, $\mathrm{V}\mathrm{A}=\mathrm{W}=J/s$.^[ref]

Absorbed electrical power $VI$ is more general than Joule heating: a capacitor can store energy, a battery can change its chemical energy, and an electrical circuit can deliver mechanical work or emit light. Even a heated resistor need not show an indefinitely rising temperature: in a thermal steady state, its dissipated power leaves by heat transfer. With the heater inside a calorimeter boundary, electrical input crosses as work; the subsequent heat transfer to the room is a different term in the first law of thermodynamics.

In his paper published in 1845, Joule connected two copper receivers with stopcocks, filled one with compressed dry air, and evacuated the other with an air pump. He immersed the connected receivers in water in an insulated arrangement, stirred the water, and read a sensitive thermometer. He then opened the stopcocks, let the air redistribute, stirred again, and compared the water's temperature with its initial value. Alternating control trials accounted for effects such as stirring and evaporation. The observation was no detectable net cooling of the common bath, rather than a record of the gas temperature at every instant. ^{[ref] [ref]}

Joule also immersed the receivers and their connecting piece in separate water vessels. The source receiver cooled while the receiving side warmed, with nearly cancelling thermal effects. ^[ref]

This distinguishes local transient changes from the final observation for the combined apparatus. Insulating its outer boundary suppresses external heat exchange; it does not prevent heat exchange between the gas, the receivers and the water inside that boundary.

An idealized modern version can use two rigid chambers joined by a valve, with thermometers in the chambers and on the walls. Prepare one chamber with gas and the other evacuated, disconnect the pump, close the apparatus to matter exchange, and let the initial temperature settle. Record initial and final equilibrium pressure and temperature, along with the wall response. Repeated closed-valve runs can reveal drift and valve-actuation effects; independent heating calibrations can estimate the heat capacity of the participating apparatus. This is a proposed measurement protocol, not a claim of a particular measured result. Fast local readings can characterize the release, but they cannot replace the final equilibrium readings in the endpoint internal energy balance.

Joule's paper On the Mechanical Equivalent of Heat (1850) describes a copper vessel holding water and a brass paddle with stationary vanes. Descending lead weights drove its shaft through strings and pulleys; the vanes opposed simple co-rotation. A boxwood shaft segment reduced thermal conduction. He measured fall distances and initial/final temperatures, repeating twenty descents per run and disconnecting the drive for rewinding. Calibrated thermometers read the water and room.^[ref]

His matched resting trials retained the water amount, duration, surroundings and reading procedure, omitting paddle motion to estimate environmental heat exchange. A screen reduced thermal radiation from his body. His calculation included the vessel and paddle heat capacities, external pulley/string losses, descent kinetic energy and string elasticity; it acknowledged residual vibration and sound.^[ref]

The measured observable is a corrected temperature rise, interpreted through the participating heat capacity; it is not a direct view of molecular motion. The experiment tests whether measured mechanical input accounts quantitatively for thermal storage. Frictional warming by itself would establish neither the conversion factor nor the absence of heat exchange. A modern authored demonstration at UCSB instead measures crank turns and a cylinder's temperature with an electrical thermometer: the apparatus differs, but again both mechanical input and thermal response must be measured. ^[ref]

The Joule-Thomson coefficient is the local temperature response to changing pressure at fixed enthalpy and fixed amount and composition:It describes the equilibrium endpoints of a Joule-Thomson effect experiment meeting the steady-flow energy balance assumptions. With $\Delta p=p_2-p_1<0$, a sufficiently small drop gives $\Delta T\simeq {\mu }_{\mathrm{JT}}\Delta p$. Thus ${\mu }_{\mathrm{JT}}>0$ means cooling, ${\mu }_{\mathrm{JT}}<0$ warming, and ${\mu }_{\mathrm{JT}}=0$ no first-order change. At zero coefficient, a finite drop can still change temperature. For a chosen illustrative local value ${\mu }_{\mathrm{JT}}=0.20\mathrm{K}\mathrm{ba}{\mathrm{r}}^{-1}$ and $\Delta p=-0.50\mathrm{bar}$, the linear prediction is $\Delta T=-0.10\mathrm{K}$; these are stipulated numbers, not measured gas properties.

For a fixed-composition simple compressible system, the measurable form isHere $C_p$ is the whole sample's heat capacity at constant pressure and $\alpha$ its volumetric coefficient of thermal expansion; alternatively use molar volume and molar heat capacity consistently. An ideal gas has $\alpha =1/T$, so ${\mu }_{\mathrm{JT}}=0$. Its enthalpy depends only on temperature; positive heat capacity at constant pressure then makes any such finite throttle preserve temperature. A real gas can have either sign. For $C_p>0$, compare $T\alpha$ with one: the thermal expansion response decides the sign, not insulation alone.^[ref]

A short derivation uses $dH=TdS+Vdp$ and the Maxwell relation $(\partial S/\partial p{)}_T=-(\partial V/\partial T{)}_p$:Setting $dH=0$ gives the coefficient. These are equilibrium state function identities, not a claim of a reversible thermodynamic process inside the throttle. For a finite drop, solve the endpoint enthalpy equality or integratealong the constant-enthalpy equilibrium curve. The coefficient can change sign during that integration, as the Van der Waals throttling model illustrates.

The Joule-Thomson effect is the temperature response of a fluid flowing from higher to lower pressure through a valve or a plug of porous medium, when the throttle is insulated and the other steady-flow energy balance assumptions hold. Its equilibrium endpoints have equal specific enthalpy. The Joule-Thomson coefficient determines whether a small drop cools or warms; cooling is not universal.

A useful contrast is between three insulated expansions. In free expansion of a gas-only closed system into a vacuum, no external work occurs and $U_2=U_1$; an ideal gas returns to its initial equilibrium temperature. In a throttle, continuous flow carries pressure work across the boundary and preserves specific enthalpy under the stated assumptions; an ideal gas again has no endpoint temperature change. In a reversible adiabatic expansion of a loaded closed system, the gas supplies work, loses internal energy and cools, even if it is an ideal gas. That process preserves entropy; throttling generally produces entropy. For a small constant-enthalpy step, $dH=TdS+Vdp=0$ gives $dS=-Vdp/T>0$ when $dp<0$ and $T,V>0$. This equilibrium comparison computes endpoint entropy differences without supplying a reversible path through the plug.

The effect is useful in refrigerators because an appropriately prepared real gas can cool while passing through a simple valve. The inlet must lie in a suitable positive-Joule-Thomson coefficient region. The Joule-Thomson inversion curve makes that requirement precise; a pressure drop by itself is not a guarantee of refrigeration.

The Joule-Thomson inversion curve is the set of equilibrium temperature–pressure states where the Joule-Thomson coefficient vanishes. For positive heat capacity at constant pressure, its condition is $T\alpha =1$, with $\alpha$ the coefficient of thermal expansion. The curve separates locally cooling and warming throttle regions. A finite isenthalpic process can cross it, so the inlet sign alone does not fix the total temperature change. An ideal gas has zero coefficient everywhere, rather than an isolated dividing curve.