I think they're ok, with maybe a few minor flaws. I guess the biggest one is that you have some continental high/low pressure centers in weird places. Those really require a pretty big landmass. Personally I tend to simplify these maps a little and just draw the ITCZ (which is the major low pressure zone in tropical areas), as well as the oceanic high pressure centers. Then, if there's a big continent similar to Eurasia I may drop a continental pressure center there, but that's about it. I tend to skip the polar areas as well, since the climate there is basically entirely dependent on temperature, so usually you don't need super-detailed information about the wind patterns. In any case, the climate in the 30-75 latitudes is usually dominated by the westerlies, unless you have something like the Siberian high going on (that is, a huge landmass).
Here's an example of my "simplistic version" for Ayesha's January (perhaps overly simplistic, it's not 100% accurate):
I usually tend to emphasize the oceanic pressure centers, since in reality the pressure difference tends to be greatest there (with the exception of the Siberian high, ofc). Also, they're probably the biggest factor affecting climate in the tropical areas. It's not that different from your version, but the big difference is that the ITCZ is not "actually" located on the Equator in January (or July, for that matter). See where it is located on Earth in January, for example:
You can see that in Summer the ITCZ makes a big southwards turn towards major landmasses which heat up a lot faster than the ocean (also, you can see how the cold currents have a big effect as well, they always cause a northwards turn). So, essentially in your case you have the continental low pressure centers and the ITCZ a bit mixed....essentially, they are almost the same thing. It's probably helpful to actually draw the ITCZ on the map, it helps to visualize the situation.