HON MSN MKG SUX LBF BGM OMA DSM NG IT MLI exk AR. NEL RAN 27 GLD TOP SSH 24 20 SPI TAD DDC 454 250 CHTS WAL 20 1. ICT RIO 26M AO 70 OKC TUL 25 D° RDU HAT 30FSM340 NKT 30 36 MEM 344 ABI GSP 35 40 * SEP B CHS 311 266. SHV MGM JAN AYS 45 RT MOB SAT LCH IAH MSY VPS AQQ JAX COF TPA

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Related questions
Question

I need hep with problem 1-3 which is shown in the second image. Please write the solution on the image or through text.

Meteorologists speak of temperatures presented in this manner as a temperature field.
Note in the second part of problem 2, that the determination of the temperatures at the unknown
points is more difficult. The reason for this is simply that there are more points to look at and more com-
binations to consider. If this seems difficult with only six points, think how it would be if you looked at a
weather map with several hundred points on it.
To alleviate this forest versus trees type of problem, meteorologists employ the useful operation known
as "isoplething." Isopleth is a Greek word meaning equal (iso)-value (pleth). Simply stated it means to
connect equal values of the particular meteorological variable with which you are working with a line. In
the case of temperature, the isopleths (which is a general term) are called isotherms and the operation can
best be explained by an example.
70
T0
70
70
13 .
70
T0
72.
130
75.-
70° F
73.
130
150
120
75
75.
77.
78.
80
80 71. 80
77.
75°F
80
80 77
80
80
Figure 1-1. Notice that in this figure the isoplething has been done at 5° intervals. That
is, there is a 70° isotherm, a 75° isotherm, and an 80° isotherm. This is not a set rule,
since isoplething can be done at any interval desired.
80°F
In most cases, the isoplething is not as simple as in the above example. Figure 1-2a shows a tem-
perature field (°F) that is more complicated.
WTL
YXL
INL
MQT
SSM
399
DLH
BTV
STC
APN
YTR
SYR
CHH
-40°
GRB
18MKG/
GERNT
BUSO
MSN
JF
SUX
23PIT HARy. PL
NEL
YNG S0
DSM
MLI
RAN
JAD
SPI.
200
25 29
OP
EC 2 HTS
RIC,
SWAL
43Gso ORF
RDU
:T
35
7 NKT HAT
30 FSM 349
GSP
MEM
34
AHN
CHS
311
MGM
H SHV
JAN
AYS
MOB
LCH
VPSAOO
JAX
MSY
IAH
TPA
Transcribed Image Text:Meteorologists speak of temperatures presented in this manner as a temperature field. Note in the second part of problem 2, that the determination of the temperatures at the unknown points is more difficult. The reason for this is simply that there are more points to look at and more com- binations to consider. If this seems difficult with only six points, think how it would be if you looked at a weather map with several hundred points on it. To alleviate this forest versus trees type of problem, meteorologists employ the useful operation known as "isoplething." Isopleth is a Greek word meaning equal (iso)-value (pleth). Simply stated it means to connect equal values of the particular meteorological variable with which you are working with a line. In the case of temperature, the isopleths (which is a general term) are called isotherms and the operation can best be explained by an example. 70 T0 70 70 13 . 70 T0 72. 130 75.- 70° F 73. 130 150 120 75 75. 77. 78. 80 80 71. 80 77. 75°F 80 80 77 80 80 Figure 1-1. Notice that in this figure the isoplething has been done at 5° intervals. That is, there is a 70° isotherm, a 75° isotherm, and an 80° isotherm. This is not a set rule, since isoplething can be done at any interval desired. 80°F In most cases, the isoplething is not as simple as in the above example. Figure 1-2a shows a tem- perature field (°F) that is more complicated. WTL YXL INL MQT SSM 399 DLH BTV STC APN YTR SYR CHH -40° GRB 18MKG/ GERNT BUSO MSN JF SUX 23PIT HARy. PL NEL YNG S0 DSM MLI RAN JAD SPI. 200 25 29 OP EC 2 HTS RIC, SWAL 43Gso ORF RDU :T 35 7 NKT HAT 30 FSM 349 GSP MEM 34 AHN CHS 311 MGM H SHV JAN AYS MOB LCH VPSAOO JAX MSY IAH TPA
However, after drawing isotherms, in figure 1-2b the field is much easier to study. It doesn't look so con-
fusing. In other words, isoplething is a means of organizing the data. Once the field has been isoplethed,
it is said that the field has been "analyzed."
WTLL
YSN
YMO
YMT
YWG
YXL
3INL
20
2539
AW
BIS
FAR
DLH
MQT
(SSM
STC
399
APN
BTV
HỌN
NTR
GRB
MSN 8MKG
GRR
29
SUX
CHH
BGM
LBF
FK
+40°+
OMA
DSM
YNG
FIT
MLI
exk
AR. PAL
NEL
RAN
.GLD
AD
TOP
SPI
20
250
SSH
DDC 454
29
Ao
CHTS
SWAL
Co
DA RIC.
ICT
20
26M
OKC TUL
TIK
RDU
NKT HAT
30FSM340
MEM
344
GSP
35
40
45
ABI
AHN
CHS
311
266
SHV
JAN
MGM
AYS
RT
LCH
MOB
SAT
IAH
MSY
VPS AQQ
JAX
VCT
COF:
ТРА
LRD
CRP
VE
BRO
063
MIA
HSUR
NQX
EYW..
Problem 1-3
Figure 1-2b
In figure 1-2b make a reasonable guess at what the temperatures are at points A, B, C, D, which are
marked with a O.
F B
F C
FD
°F
Transcribed Image Text:However, after drawing isotherms, in figure 1-2b the field is much easier to study. It doesn't look so con- fusing. In other words, isoplething is a means of organizing the data. Once the field has been isoplethed, it is said that the field has been "analyzed." WTLL YSN YMO YMT YWG YXL 3INL 20 2539 AW BIS FAR DLH MQT (SSM STC 399 APN BTV HỌN NTR GRB MSN 8MKG GRR 29 SUX CHH BGM LBF FK +40°+ OMA DSM YNG FIT MLI exk AR. PAL NEL RAN .GLD AD TOP SPI 20 250 SSH DDC 454 29 Ao CHTS SWAL Co DA RIC. ICT 20 26M OKC TUL TIK RDU NKT HAT 30FSM340 MEM 344 GSP 35 40 45 ABI AHN CHS 311 266 SHV JAN MGM AYS RT LCH MOB SAT IAH MSY VPS AQQ JAX VCT COF: ТРА LRD CRP VE BRO 063 MIA HSUR NQX EYW.. Problem 1-3 Figure 1-2b In figure 1-2b make a reasonable guess at what the temperatures are at points A, B, C, D, which are marked with a O. F B F C FD °F
Expert Solution
Step 1

A symbolic depiction which shows relationship between elements of some space like objects, themes or regions is called as maps. All sciences are directly connected or indirectly connected with the science of earth , and all types of maps can be regarded geographic on one way or the other.

Maps helps to record various facts about the earth but they are something more than this, they make a direct impact to the mind and even the unknown unseen land can be unfolded in their original form. Maps are pictorial and a glance at them is pleasant and easily brings home even  a set of complex facts in their proper relationships.

 

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