From my experience, I think in the water.
The outside curve of a stream is typically deeper than the inside curve. This occurs due to the erosion of the bank on the outer side, where the water flows faster and has more energy to remove sediment. Conversely, the inside curve experiences slower water flow, leading to sediment deposition and a shallower depth.
The outside of a meander is typically deeper than the inside. This occurs because the faster-flowing water on the outer bank erodes the riverbed more effectively, creating a deeper channel. In contrast, the slower-moving water on the inside of the meander allows sediment to accumulate, resulting in a shallower area.
The speed of water at a river bend flows much faster and deeper on the outside of the bend. On the inside of the bend the velocity is much slower and shallower.
Water outside evaporate faster.
Inside!!
Water is evaporated faster outside a refrigerator.
When a can is placed in cold water, the air inside the can cools down and contracts, creating a lower pressure inside the can compared to the outside. The higher pressure outside the can then crushes the can as it tries to equalize the pressure inside and outside.
The river is often deeper on one side of the channel due to the process of erosion and sediment deposition. As water flows, it moves faster on the outside curve of a bend, eroding the bank and creating a deeper channel. Conversely, the inside curve has slower water flow, leading to sediment deposition and a shallower area. This dynamic is part of the natural meandering process of rivers.
As the river flows around the outside of the bend, it accelerates just like when a car goes around a bend. The water, like a car, is pulled toward the outside of the bend through centripetal force (which is why road bends are often banked). The same thing happens to the water surface. It actually rises around the outside of the bend. This higher elevation of the water surface means that the water on the outside of the bend is slightly deeper than the inside. Since water always tries to seek a level surface, the water on the outside of the bend actually flows downward, along the bottom and comes back up on the inside of the bend. This secondary current pushes material from the outside of the bend back up on the inside of the bend - and that's where sand bars come from. So the combination of accelerated flow around the outside combined with the secondary current moving downward erodes the outside of the river bend.
they got the water inside by using pipes from the outside and connect them underground to the inside and let the water flow when they wanted it to.
The AC is dripping water outside because it is removing humidity from the air inside the house and expelling it outside as condensation.
the water droplets indicate that the air is cooler on one side of the glass. If the droplets are inside, then the outside is cooler. If the droplets are outside, it means the inside is cooler.