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Added code to setinfo pmodel/emodel when connected to a quakeworld server (incase anyone cares
about what version of player.mdl/eyes.mdl are being used).
QUAKE, the server now properly responds to quake1 query tools when running quake protocol.
0 for better compatibility with quake configs that
expected the gun bobbing to be off when view bobbing is off.
Fixed a crash in the "maps" command. Optimized "maps" command which was taking seconds to
execute with large numbers of files. Disabled movement prediction code on Quake servers, as it never works right without proper synchronization of moves (which only DP6/DP7/QW
protocols offer). New darkplaces engine release fixing some bugs with
.loc files that proquake accepted but darkplaces did not parse properly, no other noteworthy changes.
Many bugs fixed, some new features, fixed some map compatibility
bugs (items falling out of levels and such), fixed many
network issues (MUCH better now), some new network features (such as automatic downloads of missing files from darkplaces servers), fully updated readme
(which has been converted to HTML and posted here,
and now includes cvar and command lists), some optimizations, supports more OpenGL extensions
to accelerate stencil shadows and other features,
changed the look of rtlights to be a bit more realistic (small performance penalty).
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If you want to boost your conversion rate, creating a challenge drip campaign will be a
fresh way to engage with your audience, especially when the entire community
is involved.
Between 1920 and 1960, mean annual precipitation in the Yellow basin was 480 mm, producing a
runoff of 58 × 109 m3. The annual average sediment load was 1.6 × 109
t, with an average sediment concentration of 38 kg m−3.
Due to super-elevation of the channel belt, the contributing area of the lower basin is
only 23 000 km2 with flow along the lower reach depending on water and sediment supply
from the upper and middle basins. Water and sediment supplied by the middle
basin contribute, respectively, 50 and 88 % of the total discharges at Huayuankou which is the entrance of the lower river (Fig.
4). As the middle Yellow River basin is situated in the
fringes of the area affected by the East Asia Summer Monsoon, it suffers from frequent storms
and its annual precipitation is very sensitive to monsoonal shifts (Ye et al.
1956). Therefore, its water and sediment discharge variabilities are large.
The geography of the study area, showing the Yellow River and tributaries.
my blog ... "http://cloud-dev.Mthmn.com/node/608629 |
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