feat(render3d): the air and the light are the hour's, not one constant apiece

Aerial perspective is a curve now. A low sun shines through far more air than a
high one and shines ALONG the ground rather than down onto it, so density, height
falloff and forward scatter all ride the sun's elevation; overcast thickens the air
and flattens the scatter, because a grey sky has no disc to scatter from. `lowsun`
falls away BELOW the horizon as well as above it, or the middle of the night gets a
dawn's haze with no dawn to justify it.

The term that was missing entirely is distance DESATURATION. Blending a saturated
green ridge toward a saturated blue noon sky leaves a saturated ridge - which is why
the same valley read as a photograph at dusk, where the fog colour happened to be a
warm grey, and as a toy at one o'clock. A surface is now pulled toward its own
luminance faster than the fog itself arrives. Measured far/near saturation at the
camp: 07:00 1.11 -> 0.89, 09:00 1.04 -> 0.93, 13:00 0.98 -> 0.89.

The grade is the hour's too - nine literals bound at the draw, written by
daylight_set now. Noon is the case worth naming: direct sun is warm-white and the
only thing filling a midday shadow is a blue sky, so noon gets a cool balance over a
blue-lifted shadow with hard contrast, and dawn and dusk the reverse. Ground R-B,
lit vs shadowed: 07:00 +42.8/+14.2 -> +48.9/+15.1, 13:00 +32.2/+14.8 -> +25.2/+2.9.
Gain is left alone deliberately: the grade is `c * gain + lift * (1 - c)`, so warming
it warms the whole frame, and warming it at noon made one o'clock yellower than seven
in the morning - the opposite of the point.

The visible sky is relit. Turning a photograph on its axis does not change what
colour it was taken at, so every sunset had a mid-morning blue overhead. An analytic
sky supplies the chroma and the photograph keeps the luminance: the cloud stays where
it is and goes orange at dusk, the zenith goes deep blue at noon, and no second sky
is shipped. It fades out under the horizon and eases off under cloud.

The ground bounce follows the ground, crossing meadow to rock at the map's treeline
instead of being one green constant everywhere including above the scree.

R3D_NOAIR=1 restores all of it, so a before-and-after comes from one binary at one
hour; it joins R3D_NOCLOUD / R3D_NOSHADOW / R3D_NOGI.

Verified on macOS OpenGL, macOS Vulkan (MoltenVK) and Windows Vulkan (RTX 3070 Ti).
Backends agree: mean difference 0.15-0.88/255 within a machine. Across machines the
ORIGINAL renderer already differed by 5.02/255 at 19:12 and this build differs by
2.80, so cross-platform variance is pre-existing and did not grow. 400 frames: GL
7.4 s before and after, VK 7.0 s before and after.

Co-Authored-By: Claude Opus 5 <noreply@anthropic.com>

packages/ludic.render3d/shaders/lighting.glsl

@@ -39,6 +39,20 @@ vec2 skyUV(vec3 d) {
 // whose normal points down — the underside of a needle card, the lower half of a crown —
 // was lighting itself from that grey and came out white. Below the horizon the light is
 // what the ground reflects: the horizon sky times a meadow albedo.
+// What the ground under a surface reflects back up at it. It was one green constant for the
+// whole world, which is right in a meadow, wrong on scree, and wrong under a cliff - and on a
+// map that is not this one it is wrong everywhere. The colours are the map's now, and they
+// cross over at its treeline, so a boulder's underside up in the talus is filled with grey
+// rock light and one down by the lake is filled with green.
+// (Sampling the terrain's own albedo would be better still and wants a texture bound to every
+// program; that is phase 60's, where the terrain materials are being reworked anyway.)
+uniform vec3 u_ground_alb;       // the low ground: meadow and forest
+uniform vec3 u_ground_alb_hi;    // above the treeline: rock, scree, snow
+uniform float u_ground_hi_y;     // the height they cross at (world units)
+uniform float u_ground_hi_w;     // over how many metres
+vec3 groundAlbAt(float y) {
+  return mix(u_ground_alb, u_ground_alb_hi, smoothstep(u_ground_hi_y, u_ground_hi_y + u_ground_hi_w, y));
+}
 const vec3 GROUND_ALB = vec3(0.30, 0.34, 0.14);
 // the time of day (daylight.ludic): the sky's light scaled toward night, and the campfire
 uniform vec3 u_ibl_scale;
@@ -248,7 +262,7 @@ vec3 shade(vec3 wpos, vec3 n, vec3 albedo, float rough, float metal, float ao, f
   vec2 brdf = texture(u_brdf, vec2(NoV, rough)).rg;
   vec3 specIBL = pre * (Fr * brdf.x + brdf.y) * u_spec_scale;
   // one bounce off the sunlit ground onto whatever faces it (a warm fill from below)
-  vec3 groundAlb = vec3(0.16, 0.2, 0.07);
+  vec3 groundAlb = groundAlbAt(wpos.y) * 0.55;
   vec3 bounce = kdi * albedo * groundAlb * (u_sun_color * max(u_sun_dir.y, 0.0) / PI + irr) * clamp(0.5 - 0.5 * n.y, 0.0, 1.0) * 0.5;
   // specular occlusion from ao
   float so = clamp(pow(NoV + ao, exp2(-16.0 * rough - 1.0)) - 1.0 + ao, 0.0, 1.0);
@@ -258,7 +272,12 @@ vec3 shade(vec3 wpos, vec3 n, vec3 albedo, float rough, float metal, float ao, f
   return sane(min(c, vec3(4096.0)));
 }
 
-// aerial perspective: exponential height fog toward the horizon sky, with sun inscatter
+// aerial perspective: exponential height fog toward the horizon sky, with sun inscatter.
+// The strength of all three terms is the DAY's (daylight.ludic), not a constant: a low sun
+// is shining through far more air than a high one, and the whole look of a valley at dawn
+// is that air.
+uniform float u_fog_inscatter;   // how hard the air scatters the sun forward
+uniform float u_fog_desat;       // how fast distance takes a surface's own colour away
 vec3 applyFog(vec3 col, vec3 wpos, float dist) {
   vec3 dir = normalize(wpos - u_cam_pos);
   float hf = u_fog_height_falloff;
@@ -267,9 +286,18 @@ vec3 applyFog(vec3 col, vec3 wpos, float dist) {
   // measured from u_fog_base: two maps on one height datum, one a thousand metres lower,
   // would otherwise have that one's air exp(falloff * 1000) times thicker
   float fogAmt = u_fog_density * exp(-(u_cam_pos.y - u_fog_base) * hf) * integ;
-  float f = 1.0 - exp(-fogAmt);
+  float f = clamp(1.0 - exp(-fogAmt), 0.0, 1.0);
   vec3 fogCol = skyPrefiltered(vec3(dir.x, max(dir.y, 0.02), dir.z), 0.6);
   float sunAmt = pow(max(dot(dir, u_sun_dir), 0.0), 8.0);
-  fogCol += u_sun_color * 0.02 * sunAmt;
-  return mix(col, fogCol, clamp(f, 0.0, 1.0));
+  fogCol += u_sun_color * u_fog_inscatter * sunAmt;
+  // DISTANCE TAKES SATURATION BEFORE IT TAKES CONTRAST, and the mix below cannot do that on
+  // its own: blending a saturated green ridge toward a saturated blue sky leaves a saturated
+  // ridge. That is why the noon frame had a mountain three kilometres off reading as vividly
+  // as the workbench two metres from the camera, while the same scene at dusk - where the fog
+  // colour happens to be a warm grey - looked like a photograph. Pull the surface toward its
+  // own luminance first, faster than the fog itself arrives, and the ridge recedes at every
+  // hour rather than only at the one where the sky was already grey.
+  float l = dot(col, vec3(0.2126, 0.7152, 0.0722));
+  col = mix(col, vec3(l), clamp(f * u_fog_desat, 0.0, 1.0));
+  return mix(col, fogCol, f);
 }