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Desert Climate

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Most cited protocols related to «Desert Climate»

The experiment was performed at the Grassland Ecological Research Station of Northeast Normal University, Jilin Province, China (44°40′-44°44′N, 123°44′-123°47′E). The research station has a semi-arid, continental climate with mean annual temperature ranged from 4.6 to 6.4°C (1950–2004). Mean annual precipitation ranged from 280 to 644 mm (1950–2014) with over 70% of the precipitation occurs from June to August. Potential evapotranspiration is approximately three times that of the annual precipitation. Vegetation is dominated by L. chinensis, a C3 perennial rhizomatous grass; Phragmites australis, C. virgata and H. altissima are also abundant. Soil is classified as a chernozem soil, with 2.0% soil organic carbon content and 0.15% soil total nitrogen content (Wang et al., 2015 (link)).
One C3 perennial grass (L. chinensis) and two C4 grasses (annual: C. virgata; perennial: H. altissima) that co-occur in the meadow steppe of the study area were selected as experimental plants. L. chinensis is a widespread dominant grass of arid and semi-arid steppe in northern China, eastern Mongolia and Transbaikalia, Russia (Wang and Ba, 2008 (link)) and has an ability to resist drought, cold and alkaline conditions (Shi and Wang, 2005 (link)). C. virgata is widely distributed on the Northeast China Plain and is ecologically and economically important because of its high protein content and seed production. In addition, it also grows rapidly and is highly tolerant of alkaline conditions (Yang et al., 2008 (link); Lin et al., 2016 (link)). H. altissima is a perennial rhizomatous grass and is distributed in tropical, subtropical and temperate regions, especially in China and Southeast Asia. It has strong adaptability and stress resistance and can be used as a good soil and water conservation crop (Han et al., 2016 (link)).
On DOY 135 in 2013, seedlings of L. chinensis and H. altissima were transplanted to plastic pots (23.5 cm in diameter and 20 cm in height) filled with chernozem soil (8 kg soil pot−1). For C. virgata, plants were germinated from seeds and transplanted to plastic pots. All species were planted as monocultures (five individuals per pot). Before the initiation of the drought treatment, all the transplanted plants were manually watered (to field capacity) every 3 days. To ensure that plant growth was not limited by nutrient elements, each pot received 2 mg of nitrogen fertilizer in the form of NH4NO3 every week. All the pots were watered thoroughly on the date (DOY 165) prior to the initiation of the drought treatment. During the drought experiment period (DOY 166–172), we stopped watering the plants. Moreover, all the pots were placed under a plastic shed to exclude natural precipitation. Variations in the soil water content for the studied grasses are provided in the supplementary information (Figure S1). The measurements of leaf gas exchange and collection of both leaf dark-respired CO2 and fresh materials were conducted on DOY 166 (day 1 of the experiment), DOY 168 (day 3 of the experiment), DOY 170 (day 5 of the experiment) and DOY 172 (day 7 of the experiment). Before the initiation of the drought treatment, the studied grasses were in the stem elongation stage with average heights of 51.6, 62.9 and 42.4 cm for C. virgata, H. altissima and L. chinensis, respectively. The tiller densities of the studied grasses were 36 pot−1, 19 pot−1 and 17 pot−1 for C. virgata, H. altissima and L. chinensis, respectively. Each pot had total leaf areas of 1,045 cm2 pot−1, 618 cm2 pot−1 and 648 cm2 pot−1 for C. virgata, H. altissima and L. chinensis, respectively.
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Publication 2017
Carbon Cold Temperature Crop, Avian Desert Climate Droughts Nitrogen Nutrients Plant Development Plant Embryos Plant Leaves Plants Poaceae Proteins Rhizome Seedlings Stem, Plant

Demography: This was a cross-sectional study among 1,006 patients with symptoms of allergic disorders who were referred to the allergy clinics of Mashhad University of Medical Science from October 2010 to February 2014. Patients without any apparent symptoms were excluded. All patients were from Khorasan, a vast area located in the Northeast of Iran with a cold semi-arid to hot-arid climate with a latitude of 36º N 59º E.
A demographic checklist including information such as age, gender, and patient history was completed, and on this basis, the exact date of the allergy was deduced in order to determine the seasonal distribution of symptomology (four groups). The two most commonplace methods for determine allergens, are the skin prick test (SPT), and the radio allegro sorbent test (RAST) in vitro and in vivo methods, respectively. As the SPT method is less time consuming and more cost effective, this was selected for our study.
SPT: The SPT was performed according to the patients’ history of aeroallergen hyper-sensitivity, with applying the standard allergen extract panel (GREER, USA) and compared with histamine chloride and normal saline, respectively, as positive and negative controls. Aeroallergen extracts for SPT included outdoor extracts including Russian thistle (Salsola kali) (G59), ash (Fraxinus excelsior) (P30), grass mix (TP27), tree mix (PO714), pigweed mix (P5) and lamb’s quarter (G43) and indoor extracts such as Dermatophagoides farina (D.farina) (B64), Dermatophagoides pteronyssinus (D. pteronyssinus) (B70), cockroach (BO12), Alternaria alternate (M1), Aspergillus mix (M04), penicillium (M05), cladosporium (M13), feather (E01),and cat fur(TE3). Choosing aeroallergens were based on Flora Iranica (4 ). In the SPT, a small drop of each allergen is placed on the volar surface of the forearm. A needle (25 gage) must touch each drop and penetrate into the epidermal surface at a low angle. The tip of the needle must then be gently lifted up to raise the epidermis without any bleeding, then allergen extracts should be dropped in the pricked area separately, then after about 15–20 minutes the solution is wiped away with a cotton tissue. The SPT shows a reaction which reaches a peak for allergens. The largest and smallest diameters of each reaction were measured; the average is usually reported for the result. A wheal diameter >3 mm and a flare diameter >10 mm are considered positive results (5 ).
Statistics: Statistical analyses were performed applying SPSS for Windows (version 22, New York, USA) as well as descriptive statistics and the Chi-square test. P<0.05 was considered statistically significant.
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Publication 2017
Allegro Allergens Alternaria Aspergillus Chlorides Cladosporium Cockroaches Common Cold Dermatophagoides Dermatophagoides pteronyssinus Desert Climate Epidermis Feathers Forearm Fraxinus excelsior Gender Gossypium Histamine Hypersensitivity Needles Normal Saline Patients Penicillium Poaceae Salsola Test, Skin Tissues Touch Trees
Study locations comprised 10 field stations situated in different climatic zones viz. coastal, arid, semi-arid, mountainous and subtropical (Fig. 1). Mosquitoes were collected from army cantonments from these field stations, with the permission of Director General Armed Forces Medical Services (DGAFMS), Ministry of Defence, Government of India. From each station, indoor resting adult Cx. quinquefasciatus females were collected from different sites at dawn and dusk. Collected mosquitoes were kept in pre-sterilized cages. Mosquitoes were anesthetized with chloroform and species was identified morphologically using standard taxonomic key. Adult mosquitoes were surface sterilized with 70% ethanol for 5 min followed by washing in phosphate buffered saline (PBS) (twice) before dissection for further processing of midgut isolates and bacterial cultivation according to Pidiyar et. al.[4] (link). Midguts were microscopically dissected out under sterile conditions and transferred individually to 100 µl of brain heart infusion broth (BHI broth) in 1.5 ml microcentrifuge tubes and enriched for 4 hrs at room temperature. After enrichment, an equal volume of 40% glycerol was added in each tube and stored in liquid nitrogen and transported to the laboratory for further study. From each station, 100 mosquitoes were dissected out and midgut samples were collected for bacterial diversity. To confirm the sterility of the procedure, two controls were also taken from each station which contained PBS from a mosquito's second wash.
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Publication 2013
Adult Bacteria Brain Chloroform Culicidae Desert Climate Dissection Ethanol Glycerin Heart Military Personnel Nitrogen Phosphates Physician Executives Saline Solution Sterility, Reproductive Woman
The study was conducted in Dodoma and Morogoro regions in Tanzania. One district from each region was selected, Chamwino district in Dodoma and Kilosa district in Morogoro. Mzula and Chinoje villages in Chamwino and Tindiga and Mhenda villages in Kilosa district were selected based on factors such as geographical location, climate and consumption pattern of different indigenous vegetables (www.scale-n.org). Chamwino is located in the central plateau of Tanzania characterized by a dry Savannah and periodically semi-arid type of climate with long dry season starting late April to early December, and a short single wet season starting December to mid-April. The annual rainfall is between 350–500 mm. Kilosa District is located in eastern Tanzania characterized with sub-humid climatic condition with short rains starting in October to December and long rainfall period begin in February to May. This area has flat plains, highlands, and dry alluvial valleys with annual rainfall between 600–800 mm [13 (link)].
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Publication 2019
Climate Desert Climate Rain Vegetables
The study region is located in the southeast to northwest (~400 km) hilly transect of loess plateau in northern Shaanxi province of China (107°39′-109°15′E, 34°4′-37°31′N, altitude: 415–1,633 m a.s.l.). The region is characterized by semi-arid continental climate with an average annual rainfall of 513 mm. The mean annual air temperature is ~8.8°C. Soils in the study area are mainly derived from loess, according to the soil classification system of the Food and Agriculture Organization of the United Nations (FAO) and further classified as Calcic Cambisols (IUSS Working group WRB, 2014 (link)) with silty loam texture. A transitional environment from south to north is represented by forest, forest-grassland, and grassland to dessert grassland vegetation belts. Qingling (QL) and Ziwuling (ZWL) represent locations of mountain forests; Liandaowan (LDW) represents sites from grassland township; Guanzhong (GZ), Luanchuan (LC) and Weibei (WB) refer to agricultural areas from three Loess tablelands, respectively (Figure S1); while Ansai county (AS) and Jingbian county (JB) from regions of forest steppes (Figure S1). The codes of A, B and C following the above-mentioned site abbreviations represent various biological replicates at landscape scales. The geographical and typical vegetation characteristics of the investigated sites are as given in Table 1. In each site, three replicate subplots were randomly selected with an area of 15 m × 15 m and six replicate soil subsamples were collected from each subplot and at the soil depths of 0–10 cm using auger boring with a drill size of 20 cm length and 2 cm diameter. 6 subsamples of identical soil depths were sieved through a 2 mm mesh and then mixed to form a composite sample of ~100 g. A 10 g subsample from each plot was immediately wrapped in aluminum foil, quenched with liquid N2, and stored at −80°C laboratory conditions until the extraction of soil DNA.
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Publication 2018
Aluminum Biopharmaceuticals Desert Climate DNA Replication Drill Food Forests Training Programs

Most recents protocols related to «Desert Climate»

This experiment was conducted at the experimental field of the Xinjiang Academy of Agricultural and Reclamation Sciences (longitude 86°03’E, latitude 44°19’N) from 2020 to 2021. The test area has an arid to semiarid continental climate. The average temperature during the growth period of rice was 17.7°C and 18.7°C, and the average rainfall was 0.3 mm and 0.4 mm in 2020 and 2021, respectively. Changes in precipitation and temperature during the rice growth period (May 1 to September 30) are shown in Figure 1. The experimental soil was loam in texture with an organic matter content of 11.21 g·kg-1, total N of 0.74 g·kg-1, alkaline N of 0.61 g·kg-1, available P of 0.51 g·kg-1, and available K of 93 g·kg-1.
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Publication 2023
Desert Climate glycerol-1-nitrate Oryza sativa
The NSTM is the most developed region in Xinjiang in terms of economy, education, science, and technology, as well as an essential hub of the Silk Road Economic Belt to Central Asia and Europe (Development and Reform Commission of Xinjiang Uygur Autonomous Region 2017 ). The region is distributed in the arid and semi-arid climate zone, a typical temperate continental climate with scarce precipitation, intense evaporation, dusty weather, and large annual and daily temperature differences (Liu et al. 2018 (link)). The Taklamakan Desert, China’s largest desert, and the Gurbantunggut Desert, China’s second-largest desert, respectively, border the northern and southern slopes of the Tianshan Mountains, together with rapid urbanization in recent years, has led to serious urban and regional air pollution problems (Han 2018 (link)). Ten cities in the study area, from Hami in the east to Ili Kazakh in the west, are shown in Fig. 1 along with their locations and elevations. Table S1 provides more details on these cities, including longitude, latitude, elevation, population, GDP, and car parc.

Location of the study area. The DEM data (Shuttle Radar Topography Mission, SRTM) were downloaded from the Geospatial Data Cloud (http://www.gscloud.cn/) and processed using ArcGIS 10.2 software. a Map of China and location map of the Xinjiang deserts provided by National Tibetan Plateau Data Center (http://data.tpdc.ac.cn): I. Taklimakan Desert, II. Gurbantunggut Desert. b Enlarged topographic map of NSTM

Publication 2023
Air Pollution Climate Desert Climate Silk Urbanization

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Publication 2023
Cattle Climate Climate Change Cold Temperature Desert Climate Domestic Sheep Equus asinus Equus caballus Forests Goat Livestock Mules Poaceae Rain Tropical Climate

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Publication 2023
Cyclonic Storms Desert Climate Drainage Rain Rivers Trees
This study was conducted along a 2100-km west–east transect over arid and semi-arid regions in northern China, which exhibits a contrasting precipitation gradient from 65 to 443 mm (Figure S1). The study area covered six deserts in northern China, namely the Gurbantungut, Badangilin, Ulanbuhe, Kubuchi, Mawusu and Tengri deserts. It also covered a large diversity of vegetation and soil types (Hu et al., 2021 (link)). The dominant shrubs were Haloxylon ammodendron and Nitraria tangutorum, the dominant herbaceous plants were Agriophyllum squarrosum and Stipagrostis pennata. Our study focused on herbs in the study area, and there was significant variation in herb richness of different life form groups of herbs (2–14 herbs in total per site, average = 6.36; 2–5 perennial herbs per site, average = 3.93; 2–9 annuals per site, average = 4.21). The soil types in the study site were predominantly grey and loess, and the climate was mostly temperate continental (Hu et al., 2020 (link); Su et al., 2021 (link)).
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Publication 2023
Climate Desert Climate Menopause Plants

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More about "Desert Climate"

Arid Regions, Dry Climates, Desertification, Sahara, Mojave, Gobi, Atacama, Soil Composition, Precipitation Patterns, Vegetation Adaptations, Drought Tolerance, Evapotranspiration, Hydrology, Xerophytes, Halophytes, No. 4 filter paper, Sulfuric acid, QIAamp DNA Mini Kit, Polyethylene glycol (PEG), Qubit v2.0, PCV13, Global Positioning System, Ferric chloride, GPSMAP 62s, RNase-OFF™.
Desert climates are characterized by low rainfall, high temperatures, and sparse vegetation.
These arid regions, such as the Sahara, Mojave, Gobi, and Atacama deserts, present unique challenges for researchers studying the local ecosystems and environmental factors.
To investigate the desert climate, scientists may utilize a variety of tools and techniques.
For example, No. 4 filter paper can be used for water filtration, while sulfuric acid may be employed for soil pH analysis.
The QIAamp DNA Mini Kit can facilitate DNA extraction from desert-adapted plants and organisms, providing insights into genetic adaptations.
Polyethylene glycol (PEG) is a common reagent used in DNA precipitation, and the Qubit v2.0 fluorometer can quantify DNA and RNA concentrations.
Researchers may also leverage technologies like the Global Positioning System (GPS) to map vegetation, hydrology, and other spatial data.
The GPSMAP 62s is a handheld GPS device that can aid in field data collection.
Additionally, RNase-OFF™ can be used to inactivate RNase enzymes, ensuring the integrity of RNA samples from desert-dwelling organisms.
By utilizing these tools and techniques, scientists can gain a deeper understanding of the complex desert climate, including precipitation patterns, soil composition, and the adaptations of xerophytic and halophytic plant species.
This knowledge can inform conservation efforts, agricultural practices, and our overall understanding of arid ecosystems.