Publications by Raymond Pierrehumbert


STRATIFIED SEMIGEOSTROPHIC FLOW OVER TWO-DIMENSIONAL TOPOGRAPHY IN AN UNBOUNDED ATMOSPHERE

JOURNAL OF THE ATMOSPHERIC SCIENCES 42 (1985) 523-526

RT PIERREHUMBERT


LOCAL AND GLOBAL BAROCLINIC INSTABILITY OF ZONALLY VARYING FLOW

JOURNAL OF THE ATMOSPHERIC SCIENCES 41 (1984) 2141-2162

RT PIERREHUMBERT


LINEAR RESULTS ON THE BARRIER EFFECTS OF MESOSCALE MOUNTAINS

JOURNAL OF THE ATMOSPHERIC SCIENCES 41 (1984) 1356-1367

RT PIERREHUMBERT


FORCED COHERENT STRUCTURES AND LOCAL MULTIPLE EQUILIBRIA IN A BAROTROPIC ATMOSPHERE

JOURNAL OF THE ATMOSPHERIC SCIENCES 41 (1984) 246-257

RT PIERREHUMBERT, P MALGUZZI


OROGRAPHIC DISTORTION OF FRONTS

RIVISTA DI METEOROLOGIA AERONAUTICA 44 (1984) 249-263

RT PIERREHUMBERT


FORMATION OF SHEAR LAYERS UPSTREAM OF THE ALPS

RIVISTA DI METEOROLOGIA AERONAUTICA 44 (1984) 237-248

RT PIERREHUMBERT


BOUNDS ON THE GROWTH OF PERTURBATIONS TO NON-PARALLEL STEADY FLOW ON THE BAROTROPIC BETA-PLANE

JOURNAL OF THE ATMOSPHERIC SCIENCES 40 (1983) 1207-1217

RT PIERREHUMBERT


DYNAMICS OF WEATHER REGIMES - QUASI-STATIONARY WAVES AND BLOCKING

MONTHLY WEATHER REVIEW 110 (1982) 1105-1145

BB REINHOLD, RT PIERREHUMBERT


THE TWO-DIMENSIONAL AND 3-DIMENSIONAL INSTABILITIES OF A SPATIALLY PERIODIC SHEAR-LAYER

JOURNAL OF FLUID MECHANICS 114 (1982) 59-82

RT PIERREHUMBERT, SE WIDNALL


A family of steady, translating vortex pairs with distributed vorticity

Journal of Fluid Mechanics 102 (1981) 478-

RT Pierrehumbert

In our discussion of the behaviour of the limiting vortex pair boundary near the front stagnation point, we demonstrated that there are no solutions to the Euler equations in the half-plane x > 0 consisting of a region of constant non-zero vorticity separated from a region of irrotational flow by a straight-line boundary; from this we argued that the limiting vortex boundary must have a cusp where it contacts the negative y axis (see p. 137). However, a cusp is not the only kind of singular behaviour possible near the stagnation point. Prof. P. G. Saffman has pointed out to us that if the curvature of the boundary is allowed to become infinite at the stagnation point, the case of contact angle θO= 1/2π cannot be precluded, and further that such a solution can be found to leading order. In the rotational region we choose a stream function. © 1981, Cambridge University Press. All rights reserved.


THE STRUCTURE OF ORGANIZED VORTICES IN A FREE SHEAR-LAYER

JOURNAL OF FLUID MECHANICS 102 (1981) 301-313

RT PIERREHUMBERT, SE WIDNALL


A FAMILY OF STEADY, TRANSLATING VORTEX PAIRS WITH DISTRIBUTED VORTICITY

JOURNAL OF FLUID MECHANICS 99 (1980) 129-144

RT PIERREHUMBERT


2 AND 3 DIMENSIONAL INSTABILITIES OF A SPATIALLY PERIODIC SHEAR-LAYER

BULLETIN OF THE AMERICAN PHYSICAL SOCIETY 25 (1980) 1085-1085

RT PIERREHUMBERT, SE WIDNALL


Atmospheric circulation of tide-locked exoplanets

Annual Review of Fluid Mechanics Annual Reviews (0)

RT PIERREHUMBERT, M Hammond


GLOBAL OR LOCAL PURE-CONDENSIBLE ATMOSPHERES: IMPORTANCE OF HORIZONTAL LATENT HEAT TRANSPORT

Astrophysical Journal American Astronomical Society (0)

F Ding, RT PIERREHUMBERT

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