- Joined
- Jan 10, 2011
- Messages
- 1,468 (0.29/day)
- Location
- [Formerly] Khartoum, Sudan.
System Name | 192.168.1.1~192.168.1.100 |
---|---|
Processor | AMD Ryzen5 5600G. |
Motherboard | Gigabyte B550m DS3H. |
Cooling | AMD Wraith Stealth. |
Memory | 16GB Crucial DDR4. |
Video Card(s) | Gigabyte GTX 1080 OC (Underclocked, underpowered). |
Storage | Samsung 980 NVME 500GB && Assortment of SSDs. |
Display(s) | ViewSonic VA2406-MH 75Hz |
Case | Bitfenix Nova Midi |
Audio Device(s) | On-Board. |
Power Supply | SeaSonic CORE GM-650. |
Mouse | Logitech G300s |
Keyboard | Kingston HyperX Alloy FPS. |
VR HMD | A pair of OP spectacles. |
Software | Ubuntu 24.04 LTS. |
Benchmark Scores | Me no know English. What bench mean? Bench like one sit on? |
Should I have emphasized "on its own" in my last post?Of course it is. Every gallon which evaporates, eventually precipitates. What goes up must come down. Where do you think that water goes?
If you prefer a more scholarly viewpoint, there are numerous resources to confirm my statement, such as: Investigating the mesoscale impact of artificial reservoirs on frequency of rain during growing season - Degu - 2012 - Water Resources Research. Or The influence of large dams on surrounding climate and precipitation patterns - Degu - 2011 - Geophysical Research Letters. Both of which found small, but statistically significant increases in local precipitation due to artificial reservoirs.
There is an "effect" on local climate, but what you are proposing isn't some increase in local precipitation, you're saying that, and I quote, "most precipitation" falls near where it [evaporates]. This a volumetric comparison between evaporation and precipitation. Skimping over the papers you've linked, neither address this.
These figures are for the US. And do read the entire sentence. It continues: "and the generation-weighted average WCF by the U.S. generation mix in 2015 is estimated at 2.18 L/kWh."You didn't read the study carefully. The underlying figures are from this reference: "The generation-weighted average WCFs of thermoelectricity and hydropower are 1.25 (range of 0.18–2.0) and 16.8 (range of 0.67–1194) L/kWh, respectively.
The WCF is the water consumption factor. Hydro may be a small portion of the mix, but far more water evaporates from a hydro reservoir than other sources, meaning it contributes an outsized impact.
The composite intensity is closer to thermo's 1.25 than hydro's 16.8 because apparently the US also has hydro as a minority contributor.
My primary disagreement with Endymio's arguments is on water cycle. I may be misinterpreting, but they seem to be saying that it doesn't matter how much water we use, because it all comes back eventually. The latter is entirely true. However you can use, and in many places we are using, the accessible fresh water faster than it's being replenished.
Mass balance is the basis for how we quantify how water flows in the environment. But reducing it to merely "ins an outs" is a dangerous reductionism. Any realistic system has internal "storage" that introduce lag between said in and out (and often attenuating the former). On the long term, the volumes do equal out. On the shorter term, however, the out can be dramatically less than the in.The fact that the water equilibrium equation has ins and outs and equilibrium is maintained only if ins more or less equal the outs should be obvious to anybody with an average or above intellect.
Last edited: