I think people tend to conflate "conditions that could support life" with "we're about to find life," and those are really different things. The subsurface oceans on Europa and Enceladus do seem to have the right ingredients - liquid water, chemical energy sources, organic material - but having ingredients and actually discovering living organisms are worlds apart. We're probably looking at finding chemical hints before we find anything definitively alive, and even that's going to take some time.
The missions being developed right now like Europa Clipper are genuinely exciting, but they're mostly about reconnaissance. They'll tell us a lot more about what's actually down there - plume composition, thermal activity, potential biosignatures in the water vapor being ejected - but they're not drilling through kilometers of ice to sample the ocean itself. That's the real hurdle, and it's not a decade away. Maybe we detect something weird in the chemical data, something that doesn't fit non-biological explanations, but that's different from isolating actual microbes. I'd guess the 2030s and 2040s are more realistic for getting actual samples that might contain life, assuming funding stays consistent and the technology works as planned.
What keeps me from being too pessimistic is that we've been wrong before about where life can exist. A few decades ago, hydrothermal vents seemed like dead zones, and now we know they're teeming with life. So the conditions on these moons could absolutely support microbial life. It's just that the distance and the engineering barriers mean we're probably in the "gathering clues" phase right now, not the "we found something alive" phase. The evidence will likely come slowly, piece by piece.