我对编程相当陌生,我正在尝试在 Python 2.7 IDLE 中生成一个简单的零维能量平衡模型,以计算地球的表面温度并添加了冰反照率反馈,即模型的温度输出高于 280K,反照率保持在 0.3(30% 能量反射),如果低于 250k,反照率为 0.7(70% 能量反射,因为它的温度较低,因此地球上的冰(白色)覆盖面积更大),如果温度位于这两者之间的范围内;反照率是用公式计算的。然后从模型中运行这个新的反照率值,以提供更准确的温度。
在我的模块中我定义了;
最终气候模型 计算反照率 一个新的最终气候模型,其中考虑了新的反照率
我正在尝试制作一个图表,以比较具有不同太阳能输入但反照率一致的第一个气候模型的输出与具有不同反照率和太阳能输出的第二次运行的输出。但是不断出错;
这是我的图表脚本:
import matplotlib.pyplot as plt
import numpy as np
from EBM_IceAlbFeedback import *
# q is for the Solar Constant
q=np.linspace(2.5e26,4.0e26,150)
# t= temperature derived from the final climate model
t= finalCM(Q=q)
plt.plot(q,t,'b-')
q=np.linspace(3.0e26,4.5e26,150)
# tb= is the second set of temperatures derived from the NEWfinalCM which contains an Ice Albedo Feedback
tb= NEWfinalCM(Q=q)
plt.plot(q,tb,'r-')
plt.show ()
我的错误信息是:
Traceback (most recent call last):
File "K:/python/CompareCMsPlt2.py", line 13, in <module>
tb= NEWfinalCM(Q=q)
File "K:/python\EBM_IceAlbFeedback.py", line 228, in NEWfinalCM
NewAlb=NAlb(dist=dist, Q=Q, co2Emissions=co2Emissions, alpha=alpha, cCycleInt=cCycleInt, cCycleSlope=cCycleSlope)
File "K:/python\EBM_IceAlbFeedback.py", line 190, in NAlb
if ta>280.0:
ValueError: The truth value of an array with more than one element is ambiguous. Use a.any() or a.all()
我相信这是指我模块的这一部分中的一些内容:
def NAlb (dist=150e9, Alb=0.3, Q=3.87e26, co2Emissions=0.0, alpha=3.0, cCycleInt=0.4, cCycleSlope=0.0001):
'''
Readjusting Albedo to the output temperature
Arguments:
Q = solar ouput (W)
dist = distance from the sun (m)
co2Emissions = Cumulative CO2 emissions since 2010 (GtC)
alpha = climate sensitivity (K/2xCO2)
cCycleInt = Initial value of the airborne fraction (unitless)
cCycleSlope = Increment the airborne fraction per GtC (GtC^-1)
Return Value:
NewAlb= New Albedo (Unitless)
'''
# CALCULATE ABORTIVITY:
#Our model is baselined at an atmospheric CO2 concentration of 390 ppmv in 2010
baselineCO2=390.0
#The official IPCC figure for conversion of mass of emissions (GtC) top atmospheric concentration (ppmv)
IPCCmassToConc=2.12
#approximate correction for the carbon cycle:
cCycleAdjust=cCycleInt+cCycleSlope*co2Emissions
#convert GtC to CO2 conc in ppmv:
co2=co2Emissions*cCycleAdjust/IPCCmassToConc+baselineCO2
#calculate absorptivity
absrp=absrpFromCO2( CO2=co2, alpha=alpha )
#CALCULATE TEMPERATURE: using the same method as in the finalCM
ta=transATmCM (absrpt=absrp, dist=dist, Alb=0.3, Q=Q)
# define the thresholds for an ice free state.
if ta>280.0:
NewAlb=0.3
# define the threshold for a snow ball Earth state.
elif ta<250.0:
NewAlb=0.7# Calculate albedo for temperatures between 280k to 230k
elif 250.0<ta<280.0:
NewAlb=(0.3+(((0.7-0.3)/(280.0-250.0))*(280.0-ta)))
return NewAlb
def NEWfinalCM( co2Emissions=0.0, alpha=3., dist=150e9, Q=3.87e26, cCycleInt=0.4, cCycleSlope=0.0001 ):
'''
A New final Climate model which contains and Ice Albedo Feedback
Arguments:
Q = solar ouput (W)
dist = distance from the sun (m)
co2Emissions = Cumulative CO2 emissions since 2010 (GtC)
alpha = climate sensitivity (K/2xCO2)
cCycleInt = Initial value of the airborne fraction (unitless)
cCycleSlope = Increment the airborne fraction per GtC (GtC^-1)
Return Value:
tn = surface temperature (K)
'''
#Our model is baselined at an atmospheric CO2 concentration of 390 ppmv in 2010
baselineCO2=390.0
#The official IPCC figure for conversion of mass of emissions (GtC) top atmospheric concentration (ppmv)
IPCCmassToConc=2.12
#approximate correction for the carbon cycle:
cCycleAdjust=cCycleInt+cCycleSlope*co2Emissions
#convert GtC to CO2 conc in ppmv:
co2=co2Emissions*cCycleAdjust/IPCCmassToConc+baselineCO2
#calculate temperature
absrp=absrpFromCO2(CO2=co2, alpha=alpha)
NewAlb=NAlb(dist=dist, Q=Q, co2Emissions=co2Emissions, alpha=alpha, cCycleInt=cCycleInt, cCycleSlope=cCycleSlope)
tn=transATmCM( absrpt=absrp, dist=dist, Alb=NewAlb, Q=Q)
return tn
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谢谢