Winds aloft have no effect on the airspeed of an aircraft… only the ground speed, which is no factor at all in this issue. The indicated airspeed will be the same whether the aircraft is flying into or with a wind.
The indicated airspeed of 469 knots is near maximum for the aircraft, however at altitudes above around 25,000 feet above sea level (Flight Level 250) speeds are calculated in percentage of Mach rather than knots per hour (kph). Usual cruise speed (discounting head or tail winds which only affect ground speed) the Mach speeds average .82 Mach or so.
Additionally, although it seems anti-intuitive, winds aloft have no affect on the stall speed of any aircraft. The "stall" is an aerodynamic loss of lift usually, but not necessarily due to low airspeeds… the actual, measured speed of the aircraft through the air. What is meant is that the only thing that actually produces a stall is an angle of attack (angle of the wing to air through which it is flying) that is to great, which most often occurs at slow speeds but can occur at high speeds if the angle of attack is induced sufficiently by abrupt or aggressive elevator control input.
The elevator is the horizontal control on the tail section at the rear of the aircraft. It controls the aircraft around one of three axis… the pitch axis… that is the position of the nose up or down in relation to the horizon.
The sustainable rate of climb decreases with altitude. At sea level it can be reasonably high… say 3,000 to 5,000 feet per minute. But that requires a high deck angle (the angle of the entire aircraft as measured with the surface over which it is flying). The higher one flies the less that sustainable rate becomes to the point that the last few thousands of feet to assigned cruise altitude are often 1,000 feet per minute or less. I've seen less than 500 feet per minute in a Boeing 727 on a warm day and trying to climb a heavily loaded aircraft to 37,000 feet (Flight Level (FL) 370). (Air temperature contributes significantly to aircraft performance since it relates to the density of the air… colder air, better lift and vice versa).
Finally, ground based weather radar can actually tell the velocity of up and down drafts. Several years ago, a Lockheed 1011 landing at Dallas, Texas was caught in a "down burst" that was measured to be in excess of 10,000 feet per minute. Sadly, the aircraft was incapable of escaping from it before crashing into the surface.
Here in the Great Plains of the United States, super cells (the worst thunderstorms) often produce baseball and grapefruit sized hail (not to mention tornadoes) because of the extreme speeds of the updrafts within. Such updrafts have been known to reach 150 to 175 MPH, or about 12,000 to 15,000 feet per minute, with the added terror of having nearly as severe downdrafts adjacent to the updraft within a mile or less causing wind shear that most aircraft could not survive.
Super cells are not common in the tropics, but have been reported...