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NEW QUESTION: 1
When defining Smart Folder Templates which are considered best practices? (Choose two.)
A. If you use WebDAV or CIFS only queries returning cm:content and subtypes should be used.
B. Use FTS query language for defining the smart folder search.
C. Use Lucene query language for defining the smart folder search.
D. Use CMIS query language for defining the smart folder search.
E. Don't create filing rules that don't match the query criteria for the folder.
Answer: A,B
NEW QUESTION: 2
What is a Splunk Job? (Select all that apply.)
A. Searches that are subjected to some usage quota.
B. A child OS process manifested from the splunkd process.
C. A user-defined Splunk capability.
D. A search process kicked off via a report or an alert.
Answer: C
NEW QUESTION: 3
The Andean cordillera is made up of many interwoven mountain ranges, which include high intermundane plateaus, basins, and valleys. The Northern Andes contain several broad ecosystems falling into four altitudinal belts. Its northern subregion is distinguished by higher humidity and by greater climatic symmetry between eastern and western flanks. The Central Andes are characterized by a succession of agricultural zones with varied climatic conditions along the mountains' flanks and by large, highaltitude plateaus, variously called puna or altiplano, which do not occur in the Northern Andes. The soil fertility of the northern altiplano is generally good. The western Central Andean ranges are relatively arid with desert- like soils, whereas the eastern ranges are more humid and have more diverse soils. The eastern slopes of the Central Andes in many ways are similar to the wet forests of the Northern Andes. Unlike the Northern Andes, however, these slopes have a dry season. In regions of gentle topography, such as the Amazon basin, regional climatic variation can be determined from a few widely spaced measurements. Regional projections in the Andean cordillera are quite difficult by comparison. For example, while air temperature generally decreases with increasing altitude, variability of mountain topography can produce much lower than expected air temperatures. Nevertheless, some general climatic patterns are discernible. For example, with increasing distance south of the equator the seasonality of precipitation increases, whereas the total annual amount generally decreases. Humidity commonly increases with increasing altitude, but only to some intermediate altitude, above which it declines. The variability of mountain terrain also affects precipitation, such that conditions of extreme wetness and aridity may exist in close proximity. Related to this temperature gradient is a pattern of greater rainfall at the valley heads, and less rain at lower altitudes, resulting in part from mountain rainshadow effect. The weather patterns of the Andean cordillera and Amazon basin in general reflect movements of highand low-pressure cells associated with the Intertropical Convergence Zone, a low-pressure trough that moves further north and south on a seasonal basis.
Precipitation is high throughout the year in the highlands and on the coast in the Northern Andes. Coastal aridity increases south of central Ecuador, culminating in the Atacama desert of northern Chile. In the Central Andes, highland precipitation is seasonal, and amounts are approximately half those measured in the Northern Andes. The aridity of the Central Andean coastal zone is the result of the drying effect of the cold Pacific Humboldt current and the southern Pacific high-pressure cell. Much of the southern portion of the Central Andes in Bolivia is also arid. The dry season causes soil moisture deficits and diminished stream flow part of each year.
The passage is primarily concerned with
A. providing alternative explanations for the climatic diversity among different regions of the Andeancordillera
B. describing the climate and topography of various regions of the Andeancordillera
C. discussing the factors affecting the climate of the Andeancordillera
D. examining the effects of topography on the climate and vegetation of the Andeancordillera
E. comparing the climate and topography of the Northern Andes to those of the CentralAndes
Answer: C
Explanation:
Explanation/Reference:
Explanation:
Most of the passage - the entire second and third paragraphs - is concerned with examining the factors affecting the climate of various portions of the Andeancordillera. The first paragraph provides a framework for this discussion by describing the climate and topography of the various regions.
NEW QUESTION: 4
What is the output of the program?
#include <iostream> #include <string>
using namespace std;
class First
{
string name;
public:
First() {
name = "Alan";
}
void setName(string n) {this->name = n;}
void setName() {this->name = "John";}
void Print(){
cout << name;
}
};
int main()
{
First ob1,*ob2;
ob2 = new First();
First *t;
t = &ob1;
t->setName();
t->Print();
t = ob2;
t->setName("Steve");
ob2->Print();
}
A. It prints: AlanAlan
B. It prints: JohnSteve
C. It prints: JohnAlan
D. It prints: AlanSteve
Answer: B