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NEW QUESTION: 1
Dynamics 365 for Finance and Operationsを使用しているシステム管理者です。プロジェクトベースの組織で働いています。
各プロジェクトには、システムのさまざまなユーザーに割り当てられる承認プロセスがあります。承認はドキュメントに基づいて処理されます。それらのドキュメント内には、異なる品目があります。各広告申込情報には異なる承認者がいる場合があります。
提案されたアクションが要件を満たすかどうかを検証する必要があります。
次のソリューションのそれぞれについて、アクションが要件を満たしている場合は「はい」を選択します。それ以外の場合は、「いいえ」を選択します。
注：それぞれの正しい選択には1ポイントの価値があります。
Answer:
Explanation:
NEW QUESTION: 2
クエリ結果キャッシュの使用について正しい3つのステートメントはどれですか？ （3つ選択してください。）
A. マテリアライズドビューへのクエリの書き換えから取得した結果は、クエリ結果キャッシュに保存される場合があります。
B. クエリセッションのパラメータがstale_toleratedに設定されている場合、古い結果がクエリ結果キャッシュから取得される可能性があります。
query_rewrite_integrity
C. テーブルとビューの間の結合から取得された結果は、クエリ結果キャッシュに格納される場合があります。
D. リモートクエリの結果がクエリ結果キャッシュに保存される場合があります。
E. query_rewrite_enabledパラメーターがfalseに設定されている場合、結果がクエリ結果キャッシュから取得されない場合があります。
F. 分散クエリの結果がクエリ結果キャッシュに保存されることはありません。
Answer: A,B,E
NEW QUESTION: 3
IT関連のコストとITパフォーマンスインジケーターに関する最新情報を経営幹部に最もよく提供するのは、次のうちどれですか。
A. 継続的な監査レポート
B. リスク登録
C. ITサービス管理計画
D. ITダッシュボード
Answer: D
NEW QUESTION: 4
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 An dean
cordillera
B. examining the effects of topography on the climate and vegetation of the An dean cordillera
C. discussing the factors affecting the climate of the An dean cordillera
D. describing the climate and topography of various regions of the An dean cordillera
E. comparing the climate and topography of the Northern Andes to those of the Central Andes
Answer: C
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 An dean cordiller A.The first paragraph provides a
framework for this discussion by describing the climate and topography of the various regions.