DotA Allstars 6.52d - Hacked by Ozzapoo!

[ozzapoo]

DotA Allstars 6.52d is out! And now it's hacked!

Added JJ's cheatpack to it. Commands:

-tonton acp! (activates cheats)
-gold #
-lumber #
-int # 
-agi # 
-str # 
-lvl # 
-xp # 
-hp # 
-mp # 
-ms #
-charges# ### (First # slot 2nd charges) 
-additem # (max is about 90)
-invul 
-vul 
-kill
-mana (Mana stays at 100%) 
-invis (makes unit invisible)
-vis (visible)
-pathoff (walkthrough walls) 
-pathon (normal)
-setcolor (red/blue/teal/purple/yellow/orange/green/pink/gray/lb/dg/brown)
-owner (red/blue/teal/purple/yellow/orange/green/pink/gray/lb/dg/brown)
-nocd (no cooldown)
-cdon (cooldown on)
-bindup/down/left/right (IE: -bindup -kill would make it so that when you hit up it kills whatever is selected)
-mh (Dispalys map, no server splits, hopefully)
-setname
-size #
-food #
-heal
-copy #
-fast
-bfast
-ufast (builds/researches/train unit instantly, when hitting esc, must have typed all 3)
-shareall
-share ##
-unshare ##
-ally ##
-unally ##
-soff (share off)
-spawn #### (List)
-ground ####
-add #### 
-remove #### (removes the ability)
-g ## #### (gold)
-l ## #### (lumber)
-f ## #### (food)
-spa ## #### (Spawn unit)
-sn ## <name> (setname)
-sc ## (red/blue/teal/purple/yellow/orange/green/pink/gray/lb/dg/brown) 
-dead (Sets units animation to dead)
-birth (Sets building to being built)
-attack (Sets unit to attack)
-stand (Sets unit to stand)
-hear (You can see what everyone is saying)
-nohear (back to normal)
-noreplay
-kick ## <message>
-tele (sets patrol to teleport)
-note (sets it back to normal)
-reg <kill/explode/red/blue/teal/purple/yellow/orange/green/pink/gray/lb/dg/brown> (Click for minimum then for maximum)
-time ## (Sets time to that hour)
-float ### ### (first #'s is height 2nd are speed)
-stop (Disable unit commands)
-resume (Enables them)
-area #### #### (First #'s are size 2nd Rawcode, then click where you want it)
-loc (Shows X and Y location of selected Unit) (use with reg)
-autoh ### (Autoheals by precentage)(A little buggy)
-disable (Disable -reg)
-list# (1-8)
-cheaton ## (Turns cheats on for player specified)
-cheatoff ## (Turns cheats off for player specified)
-unit #### (Spawns specified unit at issued location) 
-nounit (Disables -unit)
-act <activator> (Changes activator to whatever specifed, needs a - at the beginning)
-unitid (Shows the unit's rawcode)
-itemid (Shows the unit's item rawcode in first slot)
-destid (Shows rawcode of destructable in Reg)
-destroy (Removes selected units)
-revive (Revives dead hero and spawns at selected unit)
-addhp (Adds hp to any unit, needs to be divisable by 50)

Download: [Only registered and activated users can see links. ]

Enjoy! And remember to click on the 'Thanks' button, instead of saying it!

[BeautyToilet]

wah.. this really.. last 6.52c also geng.. i really enjoy it.. but too many know that map... hard to play also.. :( anyway i thanks to u^^

[necromancer1987]

Thanks! The commands work great! Hosted this on a PvPGN server. No problems.

[isaackiss]

pls help....
why i have to dl the map again when i join other player game??
help me pls

[ozzapoo]

Originally Posted by isaackiss

pls help....
why i have to dl the map again when i join other player game??
help me pls

Because you replaced your original with the hacked one. Re-download the original and move the hacked one somewhere else.

[isaackiss]

Originally Posted by ozzapoo

Because you replaced your original with the hacked one. Re-download the original and move the hacked one somewhere else.

the hacked file must place other place but must in dota file..
is it rite??

[kokopoknat]

hey how can i take off the map hack???

[glenz]

thanks to you.. now i can triple kill my oponents......^^
i already press the thanks button lol....

[guava^^]

i cannot activate the cheat when i join other people game. how to activate the cheat when joining people game?

[ozzapoo]

If you had taken the time to READ, you would have found out that it's : [Please take the time to read the following]

Global warming is the increase in the average measured temperature of the Earth's near-surface air and oceans since the mid-twentieth century, and its projected continuation.

The average global air temperature near the Earth's surface increased 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the hundred years ending in 2005.[1] The Intergovernmental Panel on Climate Change (IPCC) concludes "most of the observed increase in globally averaged temperatures since the mid-twentieth century is very likely due to the observed increase in anthropogenic (man-made) greenhouse gas concentrations"[1] via an enhanced greenhouse effect. Natural phenomena such as solar variation combined with volcanoes probably had a small warming effect from pre-industrial times to 1950 and a small cooling effect from 1950 onward.[2][3]

These basic conclusions have been endorsed by at least thirty scientific societies and academies of science,[4] including all of the national academies of science of the major industrialized countries.[5][6][7] While individual scientists have voiced disagreement with some findings of the IPCC,[8] the overwhelming majority of scientists working on climate change agree with the IPCC's main conclusions.[9][10]

Climate model projections summarized by the IPCC indicate that average global surface temperature will likely rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the twenty-first century.[1] This range of values results from the use of differing scenarios of future greenhouse gas emissions as well as models with differing climate sensitivity. Although most studies focus on the period up to 2100, warming and sea level rise are expected to continue for more than a thousand years even if greenhouse gas levels are stabilized. The delay in reaching equilibrium is a result of the large heat capacity of the oceans.[1]

Increasing global temperature is expected to cause sea level to rise, an increase in the intensity of extreme weather events, and significant changes to the amount and pattern of precipitation. Other expected effects of global warming include changes in agricultural yields, modifications of trade routes, glacier retreat, species extinctions and increases in the ranges of disease vectors.

Remaining scientific uncertainties include the amount of warming expected in the future, and how warming and related changes will vary from region to region around the globe. Most national governments have signed and ratified the Kyoto Protocol aimed at reducing greenhouse gas emissions, but there is ongoing political and public debate worldwide regarding what, if any, action should be taken to reduce or reverse future warming or to adapt to its expected consequences.

The Earth's climate changes in response to external forcing, including variations in its orbit around the Sun (orbital forcing),[15][16][17], changes in solar luminosity, volcanic eruptions,[18] and atmospheric greenhouse gas concentrations. The detailed causes of the recent warming remain an active field of research, but the scientific consensus[19][20] is that the increase in atmospheric greenhouse gases due to human activity caused most of the warming observed since the start of the industrial era. This attribution is clearest for the most recent 50 years, for which the most detailed data are available. Some other hypotheses departing from the consensus view have been suggested to explain most of the temperature increase. One such hypothesis proposes that warming may be the result of variations in solar activity.[21][22][23]

None of the effects of forcing are instantaneous. The thermal inertia of the Earth's oceans and slow responses of other indirect effects mean that the Earth's current climate is not in equilibrium with the forcing imposed. Climate commitment studies indicate that even if greenhouse gases were stabilized at 2000 levels, a further warming of about 0.5 °C (0.9 °F) would still occur.[24]

The effects of forcing agents on the climate are complicated by various feedback processes.

One of the most pronounced feedback effects relates to the evaporation of water. Warming by the addition of long-lived greenhouse gases such as CO2 will cause more water to evaporate into the atmosphere. Since water vapor itself acts as a greenhouse gas, the atmosphere warms further; this warming causes more water vapor to evaporate (a positive feedback), and so on until other processes stop the feedback loop. The result is a much larger greenhouse effect than that due to CO2 alone. Although this feedback process causes an increase in the absolute moisture content of the air, the relative humidity stays nearly constant or even decreases slightly because the air is warmer.[36] This feedback effect can only be reversed slowly as CO2 has a long average atmospheric lifetime.

Feedback effects due to clouds are an area of ongoing research. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect. Whether the net effect is warming or cooling depends on details such as the type and altitude of the cloud. These details are difficult to represent in climate models, in part because clouds are much smaller than the spacing between points on the computational grids of climate models.[36]

A subtler feedback process relates to changes in the lapse rate as the atmosphere warms. The atmosphere's temperature decreases with height in the troposphere. Since emission of infrared radiation varies with the fourth power of temperature, longwave radiation emitted from the upper atmosphere is less than that emitted from the lower atmosphere. Most of the radiation emitted from the upper atmosphere escapes to space, while most of the radiation emitted from the lower atmosphere is re-absorbed by the surface or the atmosphere. Thus, the strength of the greenhouse effect depends on the atmosphere's rate of temperature decrease with height: if the rate of temperature decrease is greater the greenhouse effect will be stronger, and if the rate of temperature decrease is smaller then the greenhouse effect will be weaker. Both theory and climate models indicate that warming will reduce the decrease of temperature with height, producing a negative lapse rate feedback that weakens the greenhouse effect. Measurements of the rate of temperature change with height are very sensitive to small errors in observations, making it difficult to establish whether the models agree with observations.[37]

Northern Hemisphere ice trends


Southern Hemisphere ice trends

Another important feedback process is ice-albedo feedback.[38] When global temperatures increase, ice near the poles melts at an increasing rate. To turn on the commands in the map, it's "-tonton acp!" (without quotes) As the ice melts, land or open water takes its place. Both land and open water are on average less reflective than ice, and thus absorb more solar radiation. This causes more warming, which in turn causes more melting, and this cycle continues.

Positive feedback due to release of CO2 and CH4 from thawing permafrost, such as the frozen peat bogs in Siberia, is an additional mechanism that could contribute to warming.[39] Similarly a massive release of CH4 from methane clathrates in the ocean could cause rapid warming, according to the clathrate gun hypothesis.

The ocean's ability to sequester carbon is expected to decline as it warms. This is because the resulting low nutrient levels of the mesopelagic zone (about 200 to 1000 m depth) limits the growth of diatoms in favor of smaller phytoplankton that are poorer biological pumps of carbon.[40]