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❓:Consider the following scenario: A drummer, who practices mindfulness and believes in the power of rhythm and meditation, creates a unique rhythm pattern that repeats every T seconds. The drummer notices that when they meditate while playing this pattern, their heartbeat synchronizes with the rhythm at a certain point.1. If the rhythm pattern is represented by a trigonometric function ( R(t) = A sin(omega t) + B cos(omega t) ), where ( A ) and ( B ) are constants, and the fundamental frequency of the rhythm is ( omega = frac{2pi}{T} ), find the general solution for ( t ) when the rhythm pattern reaches a maximum while the drummer's heartbeat, represented by a function ( H(t) = C sin(lambda t + phi) ), synchronizes perfectly with the rhythm. Assume that the drummer's heartbeat has a constant frequency (lambda) and initial phase (phi).2. Given that the power of the rhythm (considered as the integral of its square over one period ( T )), ( P = int_{0}^{T} [R(t)]^2 , dt ), is directly related to the drummer's meditative state, derive the expression for ( P ) in terms of ( A ), ( B ), and ( omega ). Determine the condition under which the power of the rhythm is maximized, and explain how this aligns with the drummer's belief in the power of rhythm and meditation.
🧠:<think>Alright, so I've got this problem about a drummer who uses mindfulness and rhythm to synchronize their heartbeat. It's split into two parts. Let me tackle them one by one.Starting with part 1: We have a rhythm pattern represented by ( R(t) = A sin(omega t) + B cos(omega t) ), and the drummer's heartbeat is ( H(t) = C sin(lambda t + phi) ). We need to find when the rhythm reaches a maximum and the heartbeat synchronizes perfectly with it.First, I remember that the maximum of a sinusoidal function occurs when its derivative is zero. So, let's find the derivative of ( R(t) ) with respect to ( t ):( R'(t) = A omega cos(omega t) - B omega sin(omega t) ).To find the critical points, set ( R'(t) = 0 ):( A omega cos(omega t) - B omega sin(omega t) = 0 ).Divide both sides by ( omega ) (assuming ( omega neq 0 )):( A cos(omega t) - B sin(omega t) = 0 ).Let me rearrange this:( A cos(omega t) = B sin(omega t) ).Divide both sides by ( cos(omega t) ):( A = B tan(omega t) ).So,( tan(omega t) = frac{A}{B} ).Taking the arctangent of both sides:( omega t = arctanleft(frac{A}{B}right) + npi ), where ( n ) is an integer.Thus,( t = frac{1}{omega} arctanleft(frac{A}{B}right) + frac{npi}{omega} ).But since the function is periodic with period ( T = frac{2pi}{omega} ), the maxima will occur at intervals of ( T ). So, the general solution is:( t = frac{1}{omega} arctanleft(frac{A}{B}right) + frac{nT}{2} ).Wait, actually, the period of ( R(t) ) is ( T = frac{2pi}{omega} ), so the maxima occur every ( T ), so the general solution should be:( t = frac{1}{omega} arctanleft(frac{A}{B}right) + nT ), where ( n ) is an integer.But let me verify that. The derivative is zero at points where ( tan(omega t) = A/B ), which are spaced by ( pi/omega ). But since the function ( R(t) ) is sinusoidal, it has maxima every ( 2pi/omega ), which is the period ( T ). So, actually, the maxima occur at intervals of ( T ), so the general solution is:( t = frac{1}{omega} arctanleft(frac{A}{B}right) + nT ), ( n in mathbb{Z} ).Okay, so that's when the rhythm reaches a maximum.Now, for the heartbeat to synchronize perfectly, their frequencies must be the same. That is, ( lambda = omega ). Otherwise, they won't stay in sync. So, the condition for perfect synchronization is ( lambda = omega ).Additionally, the phase of the heartbeat should match the phase of the rhythm at the maximum point. The maximum of ( R(t) ) occurs when ( sin(omega t + phi_R) = 1 ), where ( phi_R ) is the phase shift of ( R(t) ).Wait, let me express ( R(t) ) in a different form. Since ( R(t) = A sin(omega t) + B cos(omega t) ), this can be written as ( R(t) = sqrt{A^2 + B^2} sin(omega t + phi_R) ), where ( phi_R = arctanleft(frac{B}{A}right) ) or something like that.Let me recall the identity: ( a sin x + b cos x = sqrt{a^2 + b^2} sin(x + phi) ), where ( phi = arctanleft(frac{b}{a}right) ) if ( a neq 0 ).So, in this case, ( R(t) = sqrt{A^2 + B^2} sin(omega t + phi_R) ), where ( phi_R = arctanleft(frac{B}{A}right) ).Therefore, the maximum of ( R(t) ) occurs when ( sin(omega t + phi_R) = 1 ), which is when ( omega t + phi_R = frac{pi}{2} + 2pi n ), ( n in mathbb{Z} ).So, solving for ( t ):( t = frac{pi/2 - phi_R + 2pi n}{omega} ).But ( phi_R = arctanleft(frac{B}{A}right) ). So,( t = frac{pi/2 - arctanleft(frac{B}{A}right) + 2pi n}{omega} ).Alternatively, since ( arctanleft(frac{B}{A}right) = frac{pi}{2} - arctanleft(frac{A}{B}right) ) when ( A > 0 ), this simplifies to:( t = frac{arctanleft(frac{A}{B}right) + 2pi n}{omega} ).Which matches our earlier result.Now, for the heartbeat ( H(t) = C sin(lambda t + phi) ) to synchronize perfectly, it must reach its maximum at the same time as ( R(t) ). The maximum of ( H(t) ) occurs when ( sin(lambda t + phi) = 1 ), so:( lambda t + phi = frac{pi}{2} + 2pi m ), ( m in mathbb{Z} ).At the time ( t ) when ( R(t) ) is maximum, we have:( lambda t + phi = frac{pi}{2} + 2pi m ).But we already have ( t = frac{pi/2 - phi_R + 2pi n}{omega} ).Substituting this into the equation for ( H(t) ):( lambda left( frac{pi/2 - phi_R + 2pi n}{omega} right) + phi = frac{pi}{2} + 2pi m ).Simplify:( frac{lambda}{omega} left( frac{pi}{2} - phi_R right) + frac{2pi n lambda}{omega} + phi = frac{pi}{2} + 2pi m ).For this to hold for all ( n ), the coefficients of ( n ) must match, and the constants must match.First, the coefficients of ( n ):( frac{2pi lambda}{omega} = 2pi ).Divide both sides by ( 2pi ):( frac{lambda}{omega} = 1 ) => ( lambda = omega ).So, the frequencies must be equal.Now, the constants:( frac{lambda}{omega} left( frac{pi}{2} - phi_R right) + phi = frac{pi}{2} ).But since ( lambda = omega ), this simplifies to:( left( frac{pi}{2} - phi_R right) + phi = frac{pi}{2} ).Thus,( -phi_R + phi = 0 ) => ( phi = phi_R ).So, the initial phase of the heartbeat must match the phase shift of the rhythm.Therefore, the conditions for perfect synchronization are:1. ( lambda = omega ) (same frequency)2. ( phi = phi_R = arctanleft(frac{B}{A}right) )So, the general solution for ( t ) when the rhythm reaches a maximum and the heartbeat synchronizes is when ( t = frac{pi/2 - phi_R + 2pi n}{omega} ), with ( lambda = omega ) and ( phi = phi_R ).Moving on to part 2: We need to find the power ( P ) of the rhythm, defined as the integral of its square over one period ( T ):( P = int_{0}^{T} [R(t)]^2 dt ).Given ( R(t) = A sin(omega t) + B cos(omega t) ), let's compute ( [R(t)]^2 ):( [R(t)]^2 = A^2 sin^2(omega t) + 2AB sin(omega t)cos(omega t) + B^2 cos^2(omega t) ).So,( P = int_{0}^{T} [A^2 sin^2(omega t) + 2AB sin(omega t)cos(omega t) + B^2 cos^2(omega t)] dt ).We can split this into three integrals:( P = A^2 int_{0}^{T} sin^2(omega t) dt + 2AB int_{0}^{T} sin(omega t)cos(omega t) dt + B^2 int_{0}^{T} cos^2(omega t) dt ).Let's compute each integral separately.First, ( int_{0}^{T} sin^2(omega t) dt ). Using the identity ( sin^2 x = frac{1 - cos(2x)}{2} ):( int_{0}^{T} sin^2(omega t) dt = frac{1}{2} int_{0}^{T} [1 - cos(2omega t)] dt = frac{1}{2} [T - frac{sin(2omega T)}{2omega}] ).But since ( T = frac{2pi}{omega} ), ( 2omega T = 4pi ), and ( sin(4pi) = 0 ). So,( int_{0}^{T} sin^2(omega t) dt = frac{T}{2} ).Similarly, ( int_{0}^{T} cos^2(omega t) dt = frac{T}{2} ).Now, the middle integral: ( int_{0}^{T} sin(omega t)cos(omega t) dt ). Using the identity ( sin(2x) = 2sin x cos x ), so ( sin x cos x = frac{1}{2}sin(2x) ):( int_{0}^{T} sin(omega t)cos(omega t) dt = frac{1}{2} int_{0}^{T} sin(2omega t) dt = frac{1}{2} left[ -frac{cos(2omega t)}{2omega} right]_0^T ).Compute this:( frac{1}{2} left( -frac{cos(2omega T)}{2omega} + frac{cos(0)}{2omega} right) = frac{1}{2} left( -frac{cos(4pi)}{2omega} + frac{1}{2omega} right) ).Since ( cos(4pi) = 1 ), this becomes:( frac{1}{2} left( -frac{1}{2omega} + frac{1}{2omega} right) = 0 ).So, the middle integral is zero.Putting it all together:( P = A^2 cdot frac{T}{2} + 2AB cdot 0 + B^2 cdot frac{T}{2} = frac{T}{2}(A^2 + B^2) ).But ( T = frac{2pi}{omega} ), so:( P = frac{2pi}{omega} cdot frac{1}{2}(A^2 + B^2) = frac{pi}{omega}(A^2 + B^2) ).So, the power ( P ) is ( frac{pi}{omega}(A^2 + B^2) ).To find the condition under which the power is maximized, we need to see how ( P ) depends on ( A ), ( B ), and ( omega ). Since ( omega ) is given as ( frac{2pi}{T} ), and ( T ) is the period, which is fixed for a given rhythm. However, if we consider varying ( A ) and ( B ), the power ( P ) increases as ( A^2 + B^2 ) increases. So, to maximize ( P ), we need to maximize ( A^2 + B^2 ). That is, the amplitude of the rhythm should be as large as possible.Alternatively, if ( A ) and ( B ) are fixed, then ( P ) is inversely proportional to ( omega ). So, for a fixed ( A ) and ( B ), a lower frequency ( omega ) (longer period ( T )) results in higher power.But in the context of the problem, the drummer's meditative state is directly related to the power of the rhythm. So, the drummer can increase the power by either increasing the amplitudes ( A ) and ( B ) (playing louder) or by decreasing the frequency ( omega ) (slowing down the rhythm). However, since the problem mentions that the rhythm has a fundamental frequency ( omega = frac{2pi}{T} ), I think ( T ) is fixed, so ( omega ) is fixed. Therefore, to maximize power, the drummer should maximize ( A ) and ( B ), i.e., play as loud as possible.But wait, in the problem statement, it's mentioned that the power is directly related to the meditative state. So, perhaps the drummer can adjust ( A ) and ( B ) through their playing intensity, and the more they meditate, the higher ( A ) and ( B ) become, thus increasing the power.Alternatively, if ( A ) and ( B ) are constants, then the power is fixed, but I think in the context, the drummer can vary their playing to change ( A ) and ( B ), hence affecting the power.So, the condition for maximum power is when ( A^2 + B^2 ) is maximized, which would correspond to the drummer playing with the highest possible amplitudes, aligning with their belief in the power of rhythm and meditation—essentially, the more intense the rhythm (higher amplitudes), the more powerful it is, enhancing the meditative effect.Wait, but in the expression for ( P ), it's ( frac{pi}{omega}(A^2 + B^2) ). So, if ( omega ) is fixed, then yes, maximizing ( A^2 + B^2 ) maximizes ( P ). If ( omega ) can vary, then for a given ( A ) and ( B ), lower ( omega ) (slower rhythm) would give higher power. But since the problem states that the rhythm has a fundamental frequency ( omega = frac{2pi}{T} ), I think ( omega ) is fixed, so the power is directly proportional to ( A^2 + B^2 ). Therefore, the power is maximized when ( A ) and ( B ) are as large as possible.So, summarizing part 2: The power ( P ) is ( frac{pi}{omega}(A^2 + B^2) ), and it's maximized when ( A^2 + B^2 ) is maximized, meaning the drummer plays with the highest possible amplitudes, which aligns with their belief in the power of rhythm and meditation—the stronger the rhythm, the more meditative effect it has.Final Answer1. The general solution for ( t ) when the rhythm reaches a maximum and the heartbeat synchronizes is ( t = frac{1}{omega} arctanleft(frac{A}{B}right) + nT ) with ( lambda = omega ) and ( phi = arctanleft(frac{B}{A}right) ). Thus, the solution is (boxed{t = frac{1}{omega} arctanleft(frac{A}{B}right) + nT}).2. The power of the rhythm is ( P = frac{pi}{omega}(A^2 + B^2) ), which is maximized when ( A^2 + B^2 ) is maximized. Therefore, the condition is (boxed{P = frac{pi}{omega}(A^2 + B^2)}) and it is maximized when ( A ) and ( B ) are as large as possible.</think>
❓:A nature-loving geography teacher in Las Vegas is organizing a study on the correlation between urban heat islands (UHI) and the increasing temperatures due to climate change. In particular, the teacher is focusing on how the expansion of urban areas in Las Vegas contributes to the UHI effect and subsequently, the overall temperature increase in the city. Assume the following data and parameters:1. Over the past 20 years, the urban area of Las Vegas has been expanding at an average rate of 5 square miles per year.2. The average surface temperature increase due to the UHI effect is modeled by the function ( T(U) = 0.05U + 1 ) degrees Fahrenheit, where ( U ) is the urban area in square miles.3. Additionally, the teacher has found that the regional increase in temperature due to climate change alone (excluding UHI) is modeled by the function ( C(t) = 0.02t + 0.5 ) degrees Fahrenheit, where ( t ) is the time in years.Sub-problems:1. Determine the total increase in temperature over the 20-year period considering both the UHI effect and the regional climate change. Use the given models to find the combined temperature increase after 20 years.2. Considering the teacher's concerns about climate change, calculate the rate of temperature increase per year at the end of the 20-year period due to both urban expansion and regional climate change. How does this rate compare to the initial rate of temperature increase at the start of the 20-year period?
🧠:<think>Okay, so I have this problem about a geography teacher studying the correlation between urban heat islands (UHI) and climate change in Las Vegas. The teacher is looking at how the expansion of urban areas contributes to the UHI effect and the overall temperature increase. There are two sub-problems to solve here.First, let me try to understand the given data and models.1. The urban area of Las Vegas has been expanding at 5 square miles per year over the past 20 years. So, each year, the urban area increases by 5 square miles.2. The temperature increase due to UHI is given by the function T(U) = 0.05U + 1, where U is the urban area in square miles. So, as the urban area increases, the temperature increases by 0.05 times U plus 1 degree Fahrenheit.3. The regional temperature increase due to climate change alone is modeled by C(t) = 0.02t + 0.5, where t is the time in years. So, each year, the temperature increases by 0.02t + 0.5 degrees Fahrenheit.Now, the first sub-problem is to determine the total increase in temperature over the 20-year period considering both UHI and regional climate change. So, I need to find the combined temperature increase after 20 years.Let me break this down.First, I need to model how the urban area U(t) changes over time. Since it's expanding at 5 square miles per year, starting from some initial urban area. Wait, the problem doesn't specify the initial urban area. Hmm, that might be an issue. Let me check the problem statement again.Wait, the problem says "over the past 20 years," so maybe we're considering the expansion over 20 years without an initial value? Or perhaps the initial urban area is zero? That doesn't make sense because Las Vegas must have had some urban area before the expansion started. Hmm.Wait, maybe the function T(U) is given as 0.05U + 1, so maybe U is the total urban area, not the expansion. So, if the expansion is 5 square miles per year over 20 years, the total urban area after 20 years would be 5*20 = 100 square miles. But if the initial urban area was, say, U0, then U(t) = U0 + 5t. But since the problem doesn't specify U0, maybe we can assume that U(t) is just 5t, starting from t=0. So, after 20 years, U(20) = 5*20 = 100 square miles.Alternatively, maybe the model T(U) is such that U is the expansion, not the total. Hmm, the wording says "the average surface temperature increase due to the UHI effect is modeled by the function T(U) = 0.05U + 1 degrees Fahrenheit, where U is the urban area in square miles." So, U is the urban area, not the expansion. So, if the urban area has been expanding at 5 square miles per year, then after t years, U(t) = U0 + 5t. But again, without knowing U0, we can't compute U(t). Hmm.Wait, maybe the function T(U) is given as 0.05U + 1, so perhaps U is the expansion. Wait, that might not make sense because the UHI effect depends on the total urban area, not just the expansion. Hmm.Wait, perhaps the teacher is considering the expansion over 20 years, so U(t) = 5t, where t is the time in years. So, after t years, the urban area has expanded by 5t square miles. So, at t=20, U=100 square miles. Then, the temperature increase due to UHI would be T(U) = 0.05*100 + 1 = 5 + 1 = 6 degrees Fahrenheit.But wait, is that the total increase over 20 years? Or is that the temperature increase at time t? Hmm, the function T(U) is given as a function of U, which is the urban area. So, if U increases over time, T(U) will also increase over time. So, perhaps we need to model T(U(t)) and integrate it over the 20 years or sum it up annually?Wait, the problem says "the total increase in temperature over the 20-year period considering both the UHI effect and the regional climate change." So, it's the cumulative increase, not the instantaneous rate.But both T(U) and C(t) are functions that give the temperature increase at a particular time. So, perhaps we need to compute the total increase by integrating the rate of temperature increase over the 20 years.Wait, but T(U) is given as a function of U, which is itself a function of time. So, T(U(t)) = 0.05U(t) + 1. Since U(t) = 5t, then T(U(t)) = 0.05*(5t) + 1 = 0.25t + 1. So, the temperature increase due to UHI at time t is 0.25t + 1 degrees Fahrenheit.But wait, is that the instantaneous rate or the cumulative increase? Hmm, the wording says "the average surface temperature increase due to the UHI effect is modeled by the function T(U) = 0.05U + 1 degrees Fahrenheit." So, T(U) is the total increase due to UHI when the urban area is U. So, if U increases over time, then T(U(t)) is the cumulative increase due to UHI at time t.Similarly, C(t) is the cumulative increase due to regional climate change at time t.So, the total temperature increase at time t is T(U(t)) + C(t).Therefore, at t=20, the total increase would be T(U(20)) + C(20).So, let's compute that.First, U(20) = 5*20 = 100 square miles.Then, T(U(20)) = 0.05*100 + 1 = 5 + 1 = 6 degrees.C(20) = 0.02*20 + 0.5 = 0.4 + 0.5 = 0.9 degrees.So, total increase = 6 + 0.9 = 6.9 degrees Fahrenheit.Wait, that seems straightforward. So, the total increase after 20 years is 6.9 degrees.But let me double-check if that's the correct approach. The problem says "the total increase in temperature over the 20-year period considering both the UHI effect and the regional climate change." So, it's the sum of the two effects.But wait, T(U) is the temperature increase due to UHI, which depends on the current urban area. So, as the urban area increases each year, the UHI effect increases. Similarly, the regional temperature increase is a function of time.So, if we model T(U(t)) as 0.05*(5t) + 1 = 0.25t + 1, then the UHI contribution at time t is 0.25t + 1. Similarly, C(t) = 0.02t + 0.5.So, the total temperature increase at time t is (0.25t + 1) + (0.02t + 0.5) = 0.27t + 1.5.Therefore, at t=20, total increase is 0.27*20 + 1.5 = 5.4 + 1.5 = 6.9 degrees, which matches the previous calculation.So, that seems correct.Now, the second sub-problem is to calculate the rate of temperature increase per year at the end of the 20-year period due to both urban expansion and regional climate change. How does this rate compare to the initial rate of temperature increase at the start of the 20-year period?So, we need to find the derivative of the total temperature increase with respect to time at t=20 and compare it to the derivative at t=0.Wait, but the total temperature increase is given by the sum of T(U(t)) and C(t). So, let's denote the total temperature increase as T_total(t) = T(U(t)) + C(t).Given that U(t) = 5t, so T(U(t)) = 0.05*(5t) + 1 = 0.25t + 1.C(t) = 0.02t + 0.5.Therefore, T_total(t) = 0.25t + 1 + 0.02t + 0.5 = 0.27t + 1.5.So, the rate of temperature increase is the derivative of T_total(t) with respect to t, which is dT_total/dt = 0.27 degrees per year.Wait, that's a constant rate, right? Because T_total(t) is a linear function of t, so its derivative is constant. So, the rate of temperature increase is 0.27 degrees per year throughout the entire period.Therefore, at the end of the 20-year period, the rate is 0.27 degrees per year, and at the start, it's also 0.27 degrees per year. So, the rate hasn't changed; it's the same.Wait, that seems counterintuitive because the UHI effect is increasing as the urban area expands, so I would expect the rate to increase over time. But according to the model, T(U(t)) is linear in t, and C(t) is also linear in t, so their sum is linear, meaning the rate is constant.But let me think again. The UHI effect is T(U) = 0.05U + 1. Since U is increasing at 5 square miles per year, the rate of increase of T(U) with respect to time is dT_U/dt = 0.05 * dU/dt = 0.05 * 5 = 0.25 degrees per year.Similarly, the rate of increase due to climate change is dC/dt = 0.02 degrees per year.So, the total rate is 0.25 + 0.02 = 0.27 degrees per year, which is constant over time.Therefore, the rate doesn't change; it's always 0.27 degrees per year. So, at the end of the 20-year period, the rate is the same as at the beginning.Wait, but in reality, the UHI effect might have a diminishing return or something, but according to the given model, it's linear. So, in this case, the rate is constant.So, the answer to the second sub-problem is that the rate of temperature increase per year is 0.27 degrees Fahrenheit, both at the end and the beginning of the period, so it hasn't changed.But let me make sure I'm interpreting the models correctly.The UHI effect is T(U) = 0.05U + 1. So, for each additional square mile of urban area, the temperature increases by 0.05 degrees. Since the urban area is increasing at 5 square miles per year, the UHI contribution to the temperature increase is 0.05*5 = 0.25 degrees per year.Similarly, the regional climate change contributes 0.02 degrees per year.So, adding these two, the total rate is 0.25 + 0.02 = 0.27 degrees per year, constant over time.Therefore, the rate hasn't changed; it's the same at the start and end.So, summarizing:1. Total temperature increase after 20 years: 6.9 degrees Fahrenheit.2. Rate of temperature increase per year: 0.27 degrees Fahrenheit, same at the start and end.Wait, but let me check if the total temperature increase is indeed the integral of the rate over 20 years. Since the rate is constant, the total increase would be rate * time = 0.27 * 20 = 5.4 degrees. But earlier, I calculated 6.9 degrees. Hmm, that's a discrepancy.Wait, this is a problem. Because if the rate is 0.27 per year, over 20 years, the total increase should be 0.27*20=5.4 degrees. But earlier, by plugging t=20 into T_total(t)=0.27t +1.5, I got 6.9 degrees.Wait, that suggests that T_total(t) is not just the integral of the rate, but includes some constant term. Let me see.Wait, T_total(t) = 0.27t + 1.5. So, at t=0, the temperature increase is 1.5 degrees. But according to the models, at t=0, U=0, so T(U)=1 degree, and C(0)=0.5 degrees. So, total increase at t=0 is 1 + 0.5 = 1.5 degrees, which matches.So, T_total(t) is the cumulative increase starting from t=0, which already has 1.5 degrees. Then, over 20 years, it increases by 0.27*20=5.4 degrees, so total is 1.5 +5.4=6.9 degrees.But wait, that would mean that the initial temperature increase is 1.5 degrees, and then it increases by 0.27 per year. So, the total increase over 20 years is 6.9 degrees.But the problem says "the total increase in temperature over the 20-year period." So, does that include the initial 1.5 degrees, or is it the increase from t=0 to t=20?I think it's the latter. So, the increase from t=0 to t=20 is 6.9 -1.5=5.4 degrees. Wait, but that contradicts the earlier calculation.Wait, no. Let me clarify.At t=0, the temperature increase is 1.5 degrees (from both UHI and climate change). At t=20, it's 6.9 degrees. So, the total increase over the 20-year period is 6.9 -1.5=5.4 degrees.But wait, the problem says "the total increase in temperature over the 20-year period considering both the UHI effect and the regional climate change." So, it's the cumulative increase from the start to the end, which would be 6.9 -1.5=5.4 degrees.But earlier, I thought it was 6.9 degrees. Hmm, now I'm confused.Wait, let's think about it differently. The function T(U(t))=0.25t +1 represents the temperature increase due to UHI at time t. Similarly, C(t)=0.02t +0.5 represents the temperature increase due to climate change at time t.So, the total temperature increase at time t is T(U(t)) + C(t) = (0.25t +1) + (0.02t +0.5) = 0.27t +1.5.So, at t=0, it's 1.5 degrees. At t=20, it's 0.27*20 +1.5=5.4 +1.5=6.9 degrees.Therefore, the total increase over the 20-year period is 6.9 -1.5=5.4 degrees.But wait, the problem says "the total increase in temperature over the 20-year period." So, it's the difference between the temperature at the end and the beginning, which is 5.4 degrees.But earlier, I thought it was 6.9 degrees, but that includes the initial 1.5 degrees. So, perhaps the correct answer is 5.4 degrees.Wait, but let's check the wording again: "the total increase in temperature over the 20-year period considering both the UHI effect and the regional climate change."So, it's the increase over the period, not the total temperature at the end. So, it's the difference between the temperature at the end and the start.Therefore, the total increase is 6.9 -1.5=5.4 degrees.But wait, in the first calculation, I thought of T_total(t) as the cumulative increase, but actually, it's the total temperature increase from the base level. So, the increase over the period is the difference between T_total(20) and T_total(0), which is 6.9 -1.5=5.4 degrees.Therefore, the total increase is 5.4 degrees.But then, the rate of temperature increase per year is 0.27 degrees, so over 20 years, it's 0.27*20=5.4 degrees, which matches.So, that makes sense.Therefore, the first sub-problem answer is 5.4 degrees Fahrenheit.Wait, but earlier, I thought it was 6.9 degrees, but that's the total temperature at t=20, not the increase over the period.So, the correct total increase is 5.4 degrees.Similarly, the rate of temperature increase is 0.27 degrees per year, which is constant, so it's the same at the start and end.Therefore, the answers are:1. Total increase: 5.4 degrees Fahrenheit.2. Rate of increase: 0.27 degrees per year, same at start and end.But let me double-check the models again.Given T(U) =0.05U +1. If U increases by 5 per year, then dT_U/dt =0.05*5=0.25.C(t)=0.02t +0.5, so dC/dt=0.02.Total rate: 0.25+0.02=0.27 per year.Total increase over 20 years: 0.27*20=5.4 degrees.Yes, that makes sense.So, the initial total temperature increase was 1.5 degrees, and after 20 years, it's 6.9 degrees, so the increase is 5.4 degrees.Therefore, the answers are:1. 5.4 degrees Fahrenheit.2. The rate is 0.27 degrees per year, same at the start and end.So, to summarize:1. Total temperature increase over 20 years: 5.4°F.2. Rate of temperature increase per year: 0.27°F, same at start and end.</think>
❓:A technology journalist is analyzing the performance of a distributed database system used by a global tech company. The database system consists of ( n ) servers, and each server can handle a maximum of ( m ) queries per second. The distribution of queries to the servers follows a Poisson process, where the average rate of incoming queries to the entire system is ( lambda ) queries per second.1. Given that the queries are distributed uniformly across the servers, derive an expression for the probability that a particular server becomes overloaded (i.e., receives more than ( m ) queries in one second). Assume the Poisson distribution applies to the number of queries arriving at each server.2. Suppose the technology journalist wants to ensure that no more than 5% of the time, any server is overloaded. What is the maximum value of ( lambda ) that the system can handle while maintaining this constraint? Consider ( n = 10 ) servers, each with a capacity of ( m = 20 ) queries per second.
🧠:<think>Okay, so I have this problem about a distributed database system. There are n servers, each can handle up to m queries per second. Queries are coming in at a rate of λ per second, and they're distributed uniformly across the servers. The distribution follows a Poisson process. The first part asks me to derive an expression for the probability that a particular server becomes overloaded, meaning it gets more than m queries in one second. Since the Poisson distribution applies to each server, I remember that the Poisson distribution gives the probability of a given number of events happening in a fixed interval. So, if the average rate for the entire system is λ, then each server would have an average rate of λ/n, right? Because the queries are distributed uniformly. So, the rate per server, let's call it λ_i, is λ divided by n. Therefore, the number of queries arriving at each server per second follows a Poisson distribution with parameter λ/n. The probability that a server receives more than m queries is the same as 1 minus the probability that it receives m or fewer queries. The Poisson probability mass function is P(k) = (e^{-λ_i} * (λ_i)^k) / k! for k = 0, 1, 2, ... So, the probability that a server is overloaded is:P(overload) = 1 - Σ (from k=0 to m) [ (e^{-λ/n} * (λ/n)^k) / k! ]That should be the expression. Let me write that down more neatly:P(overload) = 1 - ∑_{k=0}^{m} frac{e^{-lambda/n} (lambda/n)^k}{k!}Yeah, that seems right. So that's part 1 done.Now, part 2 is a bit more involved. The journalist wants to ensure that no more than 5% of the time, any server is overloaded. So, the probability of overload should be less than or equal to 5%, which is 0.05. We have n = 10 servers, each with m = 20 queries per second.So, we need to find the maximum λ such that P(overload) ≤ 0.05. From part 1, we have the expression for P(overload). So, we can set up the inequality:1 - ∑_{k=0}^{20} frac{e^{-lambda/10} (lambda/10)^k}{k!} ≤ 0.05Which simplifies to:∑_{k=0}^{20} frac{e^{-lambda/10} (lambda/10)^k}{k!} ≥ 0.95So, we need to find λ such that the cumulative Poisson probability up to 20 is at least 0.95. This is equivalent to finding the 95th percentile of the Poisson distribution with parameter λ/10 being less than or equal to 20.I think this is a problem where we can use the inverse of the Poisson cumulative distribution function. But since I don't have a calculator or software here, maybe I can approximate it or find a way to solve for λ.Alternatively, I can use the relationship between Poisson and normal distributions for large λ. But wait, if λ is large, the Poisson distribution can be approximated by a normal distribution with mean μ = λ/10 and variance σ² = λ/10.So, if we approximate the Poisson with a normal distribution, then the probability that a server receives more than 20 queries is approximately the probability that a normal variable with mean μ and variance σ² exceeds 20.But since we want the probability of overload to be ≤ 0.05, we can set up:P(X > 20) ≤ 0.05Which translates to:P(Z > (20 - μ)/σ) ≤ 0.05Where Z is the standard normal variable. The critical value for Z at 0.05 is approximately 1.645 (since 95th percentile is about 1.645). So,(20 - μ)/σ ≥ 1.645But μ = λ/10 and σ = sqrt(λ/10). So,(20 - λ/10) / sqrt(λ/10) ≥ 1.645Let me write that as:(20 - λ/10) ≥ 1.645 * sqrt(λ/10)Let me denote sqrt(λ/10) as t. Then, λ/10 = t², so 20 - t² ≥ 1.645 tSo, rearranging:t² + 1.645 t - 20 ≤ 0This is a quadratic inequality. Let's solve for t:t = [-1.645 ± sqrt(1.645² + 80)] / 2Compute discriminant:1.645² ≈ 2.706So, discriminant ≈ 2.706 + 80 = 82.706sqrt(82.706) ≈ 9.094So,t = [-1.645 ± 9.094]/2We discard the negative root because t is positive (sqrt(λ/10)).So,t = (-1.645 + 9.094)/2 ≈ (7.449)/2 ≈ 3.7245So, t ≈ 3.7245But t = sqrt(λ/10), so:sqrt(λ/10) ≈ 3.7245Square both sides:λ/10 ≈ (3.7245)² ≈ 13.87So, λ ≈ 13.87 * 10 ≈ 138.7So, approximately 138.7 queries per second.But wait, this is an approximation using the normal distribution. The actual Poisson distribution might give a slightly different result. Also, since we're dealing with discrete counts, the normal approximation might not be perfect, especially if λ is not very large.Alternatively, perhaps I can use the exact Poisson calculation. But without computational tools, it's a bit tedious. Maybe I can use the relationship that for Poisson, the mean is equal to the variance. So, if we set the 95th percentile to be 20, then the mean should be such that the cumulative probability up to 20 is 0.95.Alternatively, perhaps I can use the inverse Poisson function, but since I don't have that here, maybe I can use trial and error.Let me try λ = 138.7 as per the normal approximation. Then, λ/10 = 13.87.So, the Poisson parameter is 13.87. Let's compute the cumulative probability up to 20.But without a calculator, it's hard. Maybe I can use the fact that for Poisson, the cumulative distribution can be approximated or use some properties.Alternatively, perhaps I can use the relationship that for Poisson, the probability that X ≤ k is approximately equal to the normal approximation with continuity correction.Wait, maybe I should use the continuity correction. Since Poisson is discrete, when approximating with normal, we should adjust by 0.5.So, instead of P(X ≤ 20), we can approximate it as P(Y ≤ 20.5), where Y is normal with mean μ and variance σ².So, let's recast the problem with continuity correction.We have:P(X ≤ 20) ≈ P(Y ≤ 20.5)We want P(Y ≤ 20.5) ≥ 0.95So, (20.5 - μ)/σ ≥ 1.645Again, μ = λ/10, σ = sqrt(λ/10)So,(20.5 - λ/10)/sqrt(λ/10) ≥ 1.645Let me set t = sqrt(λ/10) again.So,20.5 - t² ≥ 1.645 tWhich rearranges to:t² + 1.645 t - 20.5 ≤ 0Solving quadratic:t = [-1.645 ± sqrt(1.645² + 4*20.5)] / 2Compute discriminant:1.645² ≈ 2.7064*20.5 = 82So, discriminant ≈ 2.706 + 82 = 84.706sqrt(84.706) ≈ 9.204So,t = (-1.645 + 9.204)/2 ≈ (7.559)/2 ≈ 3.7795So, t ≈ 3.7795Then, t = sqrt(λ/10) ≈ 3.7795So, λ/10 ≈ (3.7795)^2 ≈ 14.28Thus, λ ≈ 14.28 * 10 ≈ 142.8So, with continuity correction, we get λ ≈ 142.8But this is still an approximation. Let's see, maybe the exact value is somewhere around 140-145.Alternatively, perhaps I can use the exact Poisson calculation. Let's try to compute the cumulative Poisson probability for λ/10 = 14, which would be λ = 140.Compute P(X ≤ 20) when λ =14.The Poisson PMF is P(k) = e^{-14} * (14)^k /k!We need to sum from k=0 to 20.But without a calculator, it's tough, but maybe I can use some properties or known values.Alternatively, perhaps I can use the fact that for Poisson, the cumulative distribution can be related to the gamma function or incomplete gamma function, but that's beyond my current capacity without tools.Alternatively, perhaps I can use the relationship that for Poisson, the probability that X ≤ k is approximately equal to the normal approximation with continuity correction.Wait, but I already did that. Maybe I can accept that the approximate λ is around 140-145.But let's think differently. The exact value can be found by solving:∑_{k=0}^{20} e^{-λ/10} (λ/10)^k /k! = 0.95This is a transcendental equation and can't be solved analytically. So, we need to use numerical methods.But since I don't have a calculator, maybe I can use some iterative approach.Let me assume λ = 140, so λ/10 =14.Compute the cumulative Poisson probability up to 20.I know that for Poisson with λ=14, the mean is 14, and the distribution is skewed, but the cumulative up to 20 should be quite high.I recall that for Poisson, the cumulative distribution function at k=λ + z*sqrt(λ) is roughly 0.5 + Φ(z), where Φ is the standard normal CDF.But for k=20, which is 6 above the mean of 14, so z=(20-14)/sqrt(14) ≈ 6/3.7417 ≈1.603.Φ(1.603) ≈ 0.945, so the cumulative probability up to 20 would be roughly 0.945, which is close to 0.95. So, maybe λ=140 is close.But wait, actually, the exact value might be a bit higher because the normal approximation without continuity correction gives 0.945, but with continuity correction, it's slightly higher.Alternatively, if I use λ=140, the cumulative up to 20 is approximately 0.945, which is just below 0.95. So, perhaps we need a slightly higher λ.Let me try λ=142, so λ/10=14.2Compute the cumulative Poisson up to 20.Using the same method, z=(20 -14.2)/sqrt(14.2) ≈5.8/3.768≈1.539Φ(1.539)≈0.938, which is lower than 0.95. Wait, that can't be.Wait, no, actually, the z-score is (20 - μ)/σ, so for μ=14.2, σ≈3.768, so z=(20-14.2)/3.768≈5.8/3.768≈1.539Φ(1.539)≈0.938, so cumulative up to 20 is about 0.938, which is less than 0.95. So, we need a higher μ.Wait, but as μ increases, the cumulative up to 20 will decrease because the distribution shifts to the right. Wait, no, actually, if μ increases, the probability that X ≤20 decreases because the mean is moving away from 20.Wait, that seems contradictory. Let me think again.If μ increases, the Poisson distribution shifts to the right, so the probability that X ≤20 decreases. So, to get a higher cumulative probability up to 20, we need a lower μ.Wait, but we want the cumulative up to 20 to be at least 0.95. So, if at μ=14, cumulative is ~0.945, which is just below 0.95. So, maybe we need a slightly lower μ to get cumulative up to 20 to be 0.95.Wait, but that contradicts the earlier approximation. Hmm.Alternatively, perhaps I'm confusing the direction. Let me think again.If μ is higher, the distribution is shifted right, so the probability that X ≤20 decreases. So, to have a higher cumulative probability up to 20, we need a lower μ.But wait, we want the cumulative up to 20 to be at least 0.95. So, if at μ=14, cumulative is ~0.945, which is just below 0.95, so to increase the cumulative, we need to decrease μ.Wait, that doesn't make sense because decreasing μ would make the distribution shift left, increasing the cumulative up to 20.Wait, yes, that's correct. So, if μ=14 gives cumulative ~0.945, then to get cumulative=0.95, we need a slightly lower μ.Wait, but that contradicts the earlier normal approximation which suggested μ=14.28.I think I'm getting confused here. Let me clarify.We have two approaches:1. Normal approximation without continuity correction: gave μ≈13.87, λ≈138.72. Normal approximation with continuity correction: gave μ≈14.28, λ≈142.8But when I tried μ=14, the cumulative up to 20 was ~0.945, which is close to 0.95. So, perhaps the exact value is around μ=14, λ=140.But let's think about the exact Poisson calculation.The exact cumulative Poisson probability for k=20, λ=14 can be computed as:P(X ≤20) = e^{-14} * Σ_{k=0}^{20} (14^k)/k!This is a bit tedious, but maybe I can use some properties or known values.Alternatively, perhaps I can use the fact that for Poisson, the cumulative distribution function can be expressed in terms of the incomplete gamma function:P(X ≤k) = Γ(k+1, λ)/k!Where Γ is the upper incomplete gamma function.But without computational tools, it's hard to compute.Alternatively, perhaps I can use the relationship that for Poisson, the probability that X ≤k is approximately equal to the normal approximation with continuity correction.Wait, but I already tried that.Alternatively, perhaps I can use the fact that for Poisson, the probability that X ≤k is approximately equal to the normal approximation with continuity correction, which would give us:P(X ≤20) ≈ Φ( (20.5 - μ)/σ )We want this to be ≥0.95, so:(20.5 - μ)/σ ≥1.645With μ=λ/10, σ= sqrt(λ/10)So,(20.5 - λ/10)/sqrt(λ/10) ≥1.645Let me denote t = sqrt(λ/10), so λ/10 = t²So,20.5 - t² ≥1.645 tRearranged:t² +1.645 t -20.5 ≤0Solving quadratic:t = [-1.645 ± sqrt(1.645² +4*20.5)] /2Compute discriminant:1.645² ≈2.7064*20.5=82So, discriminant≈2.706+82=84.706sqrt(84.706)≈9.204So,t=(-1.645 +9.204)/2≈(7.559)/2≈3.7795Thus, t≈3.7795So, t= sqrt(λ/10)=3.7795Thus, λ/10≈(3.7795)^2≈14.28So, λ≈142.8Therefore, the maximum λ is approximately 142.8.But earlier, when I tried μ=14 (λ=140), the cumulative was ~0.945, which is just below 0.95. So, to get to 0.95, we need a slightly higher μ, which would require a slightly higher λ.Wait, but according to the continuity correction, we need λ≈142.8.But let's check what happens when μ=14.28 (λ=142.8). Then, the cumulative up to 20 would be:Using normal approximation with continuity correction:z=(20.5 -14.28)/sqrt(14.28)≈(6.22)/3.78≈1.645Which is exactly the critical value for 0.95. So, the cumulative probability up to 20.5 is 0.95, which corresponds to the cumulative up to 20 being approximately 0.95.Therefore, the exact value of λ is approximately 142.8.But since we can't have a fraction of a query, we might round it down to 142 or up to 143.But the question asks for the maximum λ that the system can handle while maintaining the constraint. So, we need to ensure that the cumulative up to 20 is at least 0.95.Therefore, the maximum λ is approximately 142.8, which we can write as 142.8, but since λ is in queries per second, it's a continuous variable, so we can express it as 142.8.But let me check if λ=142.8 gives cumulative up to 20 as exactly 0.95.Using the normal approximation with continuity correction, yes, it does.But in reality, the exact Poisson cumulative might be slightly different. However, without computational tools, this is the best approximation we can do.Therefore, the maximum λ is approximately 142.8.But let me think again. If I set λ=142.8, then λ/10=14.28.The cumulative Poisson up to 20 is approximately equal to the normal CDF at 20.5, which is 0.95.Therefore, the exact value is around 142.8.So, rounding to a reasonable number, perhaps 143.But the question doesn't specify rounding, so we can present it as 142.8.Alternatively, if we use the exact Poisson calculation, it might be slightly different, but without computational tools, we can't get the exact value.Therefore, the maximum λ is approximately 142.8.So, to sum up:1. The probability that a server is overloaded is 1 - sum from k=0 to m of (e^{-λ/n} (λ/n)^k)/k!2. The maximum λ is approximately 142.8, which we can write as 142.8.But let me check if I made any mistakes in the reasoning.Wait, when I used the normal approximation without continuity correction, I got λ≈138.7, and with continuity correction, λ≈142.8. The exact value is somewhere in between, but closer to 142.8.Therefore, the maximum λ is approximately 142.8.But let me think about the units. The rate is per second, so it's fine.Therefore, the final answer is approximately 142.8.But to be precise, perhaps I should use more decimal places.But since the problem didn't specify, I think 142.8 is acceptable.Alternatively, if I use the exact Poisson calculation, perhaps the value is slightly different, but without computational tools, we can't get the exact value.Therefore, the maximum λ is approximately 142.8.</think>
❓:Imagine a gallery dedicated to minimalist, black-and-white design aesthetics. The gallery consists of a continuous series of n identical rectangular rooms arranged linearly. Each room is painted entirely in either black or white. The art director wants to install a unique light fixture in each room such that the intensity of light in each room is proportional to the Fibonacci sequence, ensuring a harmonious progression that aligns with minimalist principles.1. Given that the intensity of light in the first room is F(1) = 1 and the second room is F(2) = 1, where F(k) denotes the k-th Fibonacci number, derive a formula for the light intensity in the k-th room, F(k), for k ≥ 3. Determine the general expression for the total intensity of light across all n rooms.2. Suppose the art director decides that the total intensity of light in the gallery should not exceed 10,000 units. Find the maximum number of rooms, n, that can be arranged while adhering to this constraint, and determine the color arrangement (black or white) such that the transition between room colors maximizes the aesthetic appeal, defined as the number of transitions between black and white rooms. Assume the sequence of colors starts with a black room.
🧠:<think>Alright, so I have this problem about a gallery with n identical rectangular rooms arranged linearly. Each room is painted either black or white, and each has a unique light fixture whose intensity follows the Fibonacci sequence. The first room has intensity F(1) = 1, the second F(2) = 1, and so on. The first part asks me to derive a formula for F(k) for k ≥ 3 and find the total intensity across all n rooms. Hmm, okay. I remember the Fibonacci sequence is defined such that each term is the sum of the two preceding ones. So, F(k) = F(k-1) + F(k-2) for k ≥ 3. That seems straightforward. So, the general formula for F(k) is just the standard Fibonacci recurrence relation. Now, for the total intensity, I need to sum up F(1) + F(2) + ... + F(n). I recall that the sum of the first n Fibonacci numbers has a closed-form expression. Let me try to remember or derive it.I know that the sum S(n) = F(1) + F(2) + ... + F(n). Using the recurrence relation, each term F(k) = F(k-1) + F(k-2). So, maybe I can express S(n) in terms of previous sums.Let's write out the sum:S(n) = F(1) + F(2) + F(3) + ... + F(n) = 1 + 1 + (1+1) + (1+2) + ... + F(n)Wait, maybe there's a better way. I remember that the sum of the first n Fibonacci numbers is equal to F(n+2) - 1. Let me verify that.For n=1: S(1)=1. F(3)=2, so 2-1=1. Correct.For n=2: S(2)=1+1=2. F(4)=3, 3-1=2. Correct.For n=3: S(3)=1+1+2=4. F(5)=5, 5-1=4. Correct.Okay, so it seems that S(n) = F(n+2) - 1. So, that's the formula for the total intensity.Moving on to the second part. The total intensity shouldn't exceed 10,000 units. So, we need to find the maximum n such that S(n) = F(n+2) - 1 ≤ 10,000.Also, we need to determine the color arrangement starting with black, maximizing the number of transitions between black and white. So, the color sequence should alternate as much as possible.Since the sequence starts with black, the optimal color arrangement would be black, white, black, white, etc., to maximize transitions. So, the number of transitions would be n-1 if n is odd, or n-1 if n is even? Wait, no. If you alternate starting with black, the number of transitions is n-1 regardless of whether n is odd or even because each adjacent pair alternates. For example, n=1: 0 transitions; n=2: 1 transition; n=3: 2 transitions, etc. So, the maximum number of transitions is n-1.But wait, the problem says "maximizes the aesthetic appeal, defined as the number of transitions between black and white rooms." So, yes, starting with black and alternating each time gives the maximum number of transitions, which is n-1.So, first, I need to find the maximum n such that F(n+2) - 1 ≤ 10,000. So, F(n+2) ≤ 10,001.I need to compute Fibonacci numbers until I exceed 10,001.Let me list the Fibonacci numbers:F(1) = 1F(2) = 1F(3) = 2F(4) = 3F(5) = 5F(6) = 8F(7) = 13F(8) = 21F(9) = 34F(10) = 55F(11) = 89F(12) = 144F(13) = 233F(14) = 377F(15) = 610F(16) = 987F(17) = 1597F(18) = 2584F(19) = 4181F(20) = 6765F(21) = 10946F(22) = 17711So, F(21) = 10946, which is greater than 10,001. So, F(n+2) must be ≤ 10,001. So, the largest F(n+2) ≤ 10,001 is F(20) = 6765.Wait, but 6765 is F(20). So, n+2 = 20, so n=18.Wait, but let's check:If n=18, then S(n) = F(20) -1 = 6765 -1 = 6764, which is less than 10,000.If n=19, S(n)=F(21)-1=10946 -1=10945, which is more than 10,000.So, the maximum n is 18.But wait, let me confirm:Wait, F(21)=10946, so S(19)=10946 -1=10945>10,000.So, n=18 gives S(18)=F(20)-1=6765-1=6764.But wait, 6764 is much less than 10,000. Maybe I can go higher.Wait, perhaps I made a mistake in the formula. The total intensity is S(n)=F(n+2)-1. So, if n=18, S(n)=F(20)-1=6765-1=6764.n=19: S(n)=F(21)-1=10946-1=10945>10,000.But wait, 10,000 is the limit. So, n=19 gives 10,945 which is over, so n=18 is the maximum.But wait, is there a way to have n=19 but with some rooms having lower intensity? But no, the intensity is fixed as Fibonacci numbers starting from F(1)=1, so each room must have F(k) intensity. So, you can't skip or reduce any intensity.Therefore, the maximum n is 18.But wait, let me check again.Wait, n=18: total intensity is 6764, which is under 10,000. Maybe n=19 is too much, but perhaps n=20?Wait, n=20: S(n)=F(22)-1=17711-1=17710>10,000.So, n=18 is the maximum.But wait, 10,000 is the limit. So, n=18 gives 6764, which is way under. Maybe I can go higher. Wait, perhaps I miscalculated the Fibonacci numbers.Wait, let me list them again up to F(25):F(1)=1F(2)=1F(3)=2F(4)=3F(5)=5F(6)=8F(7)=13F(8)=21F(9)=34F(10)=55F(11)=89F(12)=144F(13)=233F(14)=377F(15)=610F(16)=987F(17)=1597F(18)=2584F(19)=4181F(20)=6765F(21)=10946F(22)=17711F(23)=28657F(24)=46368F(25)=75025So, F(21)=10946, which is greater than 10,001. So, n+2=21 would give S(n)=10946-1=10945>10,000.So, n+2=20 gives S(n)=6765-1=6764.But wait, 6764 is much less than 10,000. Maybe I can find a higher n where F(n+2)-1 ≤10,000.Wait, F(21)=10946, which is over. So, the previous one is F(20)=6765, which is under. So, n+2=20, so n=18.But wait, 6765 is F(20), so n=18 gives S(n)=6764.But 6764 is much less than 10,000. Is there a way to have a higher n?Wait, perhaps I made a mistake in the formula. Let me double-check.The sum S(n) = F(1) + F(2) + ... + F(n) = F(n+2) - 1.Yes, that's correct. So, for n=18, S(n)=F(20)-1=6765-1=6764.n=19: S(n)=F(21)-1=10946-1=10945>10,000.So, n=18 is the maximum.But wait, 6764 is way under 10,000. Maybe I can have a higher n by adjusting the color arrangement? Wait, no, the color arrangement affects the transitions but not the intensity. The intensity is fixed as Fibonacci numbers regardless of color. So, the total intensity is fixed once n is chosen.Therefore, the maximum n is 18.But wait, let me check if n=19 is possible. S(n)=10945>10,000, so it's over. So, n=18 is the maximum.Now, for the color arrangement, starting with black, and alternating as much as possible to maximize transitions. So, the sequence would be B, W, B, W, ..., ending with B if n is odd, or W if n is even.Since n=18 is even, the last room would be white. So, the color sequence is B, W, B, W, ..., W.Number of transitions is n-1=17.So, the maximum number of rooms is 18, with a color arrangement alternating starting with black, resulting in 17 transitions.Wait, but let me confirm the number of transitions. For n=18, starting with B, the sequence is B, W, B, W,..., ending with W. So, each adjacent pair alternates, so transitions are between each pair. So, for n=18, there are 17 transitions.Yes, that's correct.So, summarizing:1. F(k) = F(k-1) + F(k-2) for k ≥ 3. Total intensity S(n) = F(n+2) - 1.2. Maximum n is 18, with color arrangement alternating starting with black, resulting in 17 transitions.</think>