Mountain tops reaching above 8000m in the inner domain (d04) of the simulation: Mount Everest, Kanchanjunga, Lhotse, Makalu and Cho Oyu. OpenWeather products are all ready-to-use and allow to minimise customers . The threshold wind speed, below which reliable measurements cannot be obtained, for the anemometers measuring at all three stations is 0.21 m s 1 for wind speed and 0.15 m s 1 for wind direction. The model evaluation is based on the mean bias error (MBE), mean absolute error (MAE) and root-mean-square error (RMSE) (Inness and Dorling,2012) of the 2m temperature and 5m wind speed. OpenWeather is a team of IT experts and data scientists that has been practising deep weather data science since 2014. 167 pulls off upset as play suspended due to heat. Soc., 95, 10211028, and Land Surface Datasets, Atmosphere, 9, 196, https://doi.org/10.3390/atmos9050196, 2018.a, Serafin, S. and Zardi, D.: Daytime Heat Transfer Processes Related to Slope Bonaf, U., Calzolari, F., Colombo, T., Decesari, S., DiBiagio, C., 8-day weather forecast with Wind, Humidity, Dew Point, Pressure, Cloudiness, Precipitation, Visibility, and UV Index. Now in this section, we will see how to access weather data. (2002) describe the seasonal variation and climatology of the study area by means of 6years of meteorological observations made at the Nepal Climate Observatory Pyramid (NCO-P) station, located close to the base of Mount Everest (marked as a black star in Fig.2b). Lets implement it practically in python . After 60 grid points (approximately 60km) into the valley, the valley floors start to incline towards the valley top. The plain-to-valley winds flow over the 1000m high barrier at the entrances to the Gaurishankar and Khumbu valleys in a shallow layer of less than 500m (grid points 110130 in Gaurishankar and grid points 120140 in Khumbu). In this way, the structure of the flow in plainvalley interaction can be studied more successfully (cross-sections are discussed later in Sect.4.2). In the morning (20December at 09:00LT 2h and 10min after sunrise), the valley atmospheres are mainly characterised by weak up-valley winds (Fig.8). Welcome to OpenWeatherMapAPI Python tutorial. For example: Winds %wind-speed% Km/h^ with gusts up to %wind-gust% Km/h^ With wind gust data this will convert to: Winds 10 Km/h with gusts up to 20 Km/h Subscribe to the new subscription plan "One Call by Call" and get all weather data for any coordinates with a single API call. 850614).Open-access funding was provided by the Helsinki University Library. During the simulated 4d, the daytime up-valley winds vary between the valleys and their parts, with respect to both strength and flow depth. The third aim is to attempt to explain the causes for the differences in the local winds. We first analysis the large-scale flow to ensure that it is consistent with the analysis in ERA5 (discussed in Sect.2.1). Soc., 91, 10151058, You can call by city name or city name, state code and country code. A., Soci, C., Abdalla, S., Abellan, X., Balsamo, G., Bechtold, P., Biavati, Atmospheric temperature below which water droplets begin to condense and dew can form, C. At the top of the Gaurishankar and Khumbu valleys, the depth of the up-valley wind layer decreases to a few hundred metres, although it still extends all the way to the top of the valleys (Fig.S4b and d in the Supplement). To get data in XML format just set up mode = xml. The daytime up-valley winds are connected to the plain by winds that propagate over this topographical barrier, so it is reasonable to follow this line in the analysis (discussed further in Sect.4). In all of the valleys during the 4d simulation, both the vertical extent of the diurnal cycle of potential temperature and the layer of up-valley winds is deepest in the lower parts of the valleys (yellow and purple crosses in Figs.9 and 11). Am. Model Dev., 14, 14271443. Is there a configuration to retrieve the speed as km/h? The grid points on both slopes are selected to have the same elevation gain with respect to the valley centre line height and, thus, can differ regarding their horizontal distance from the centre line. In the four valleys, the ridge heights also increase along the valley, meaning that the valley floor inclination does not necessarily lead to a reduction in the volume of the valley atmosphere. Enhance your short-term planning with Road Risk API by exploiting an accurate minute-by-minute forecast for 2 hours, hourly weather forecast and national alerts for five-days. So you just need to put the units in your label to display it properly. Get the API keys. Cross-valley width at an elevation of 1000m above the valley centre line is shown using the blue line. See EXAMPLE.md for a demonstration of how I use these in my Daily Template. The version used in this study is WRF3.6.1. The valley depth is described as the height difference between the centre line and average of the ridgelines (shown in purple). For each point on the globe, OpenWeather provides historical, current and forecasted weather data via light-speed APIs. %wind-gust% This data is only returned by the API if the condition exists. OpenWeatherMapAPI Python Tutorial Getting Started With OpenWeatherMap API, OpenWeatherMapAPI Python Tutorial -Access Current Weather Data For One Location, "http://api.openweathermap.org/data/2.5/weather? To access data by zip code, you have to pass zip code and country code parameters. The wind speed above this location, 200m higher than the model level that is shown in Fig.6, is already reduced by half (not shown). Chem. Am. J. Recent policy changes limit the API access for new registered users with a free plan, they should select the `hourly` mode. The buoyancy mechanism drives shallower and weaker winds, such as the typical cross-valley slope winds, compared with the valley wind mechanisms. Figure10Vertical cross-section of potential temperature change above the valley centre lines (yellow lines in Fig.2b) between 09:00 and 15:00LT on20December (a, c, e, g) and 21December (b, d, f, h). Figure6Along-valley wind velocity in different parts of each of the four valleys (crosses of the same colours in Figs.2 and 3) on the fourth model level (approximately 300m above the surface). List of weather condition codes with icons If you do not see some of the parameters in your API response it means that these weather phenomena are just not happened for the time of measurement for the city or location chosen. Interactive weather map allows you to watch for current temperature and weather conditions in your city or any . See EXAMPLE.md for a demonstration of how I use this in my Daily Template. The OpenWeatherMap weather integrations uses OpenWeatherMap as a source for current meteorological data for your location. The up-valley wind speeds vary from 2 to 10ms1 in the afternoon (described in detail in Sect.4.1). Ek, M., Meng, J., Wei, H., Yang, R., Lord, S., vanden Dool, H., Kumar, A., In Makalu Valley, the valley floor elevation increases from 500 to 4000ma.s.l. If you register an new API key with OpenWeatherMap, it will be activated automatically, this typically takes between 10 minutes and 2 hours You, or anyone with the link, can use it to retrieve your Cart at any time. Earlier this month, organiser Craig Tiley slammed claims the Open should be rescheduled for a cooler time of year. weather analysis and forecasting/16th conference on numerical weather The same analysis with an extended yscale to show the along-valley wind velocities less than 5ms1 is shown in the Supplement (Fig.S2). 3. The wind component describing the cross-valley winds at the slopes located around the ith grid point in the valley centre line is calculated using Eq.(5): The four valleys considered in this study and their centre lines identified by the algorithm described in Sect.2.3.1 are marked using yellow lines in Fig.2b. Easy to install instructions and includes mounting bracket and hardware. Here, (xi,yi) denote the coordinates of the ith grid point on the valley centre line in the inner model domain grid. Thompson, G., Field, P.R., Rasmussen, R.M., and Hall, W.D.: Explicit The along-valley winds at night are weak in all four valleys and generally remain in the up-valley direction (night-time is shown using shading in Fig.6). To determine if the large-scale flow during our 4d period is representative of the long-term climatology, we compare daily averages of upper-level winds from the study period to the 40-year climatology using the ERA5 reanalysis (Hersbach etal.,2020). forecast.windSpeed.mps Wind speed, meters per second; forecast.windSpeed.unit Unit of measurements; forecast.windSpeed.name Type of the wind; forecast.windGust. For more details about pretty print JSON data check this. The local wind patterns in Khumbu Valley (one of the valleys that is investigated in this study) have been studied in the past by means of meteorological observations (Inoue,1976; Ueno and Kayastha,2001; Bollasina etal.,2002; Ueno etal.,2008; Bonasoni etal.,2010; Shea etal.,2015; Yang etal.,2018) and high-resolution meteorological modelling (Karki etal.,2017; Potter etal.,2018, 2021). Water Resour. Brutal conditions saw the heat policy enforced on a scorching day at Melbourne Park, with play halted around 2pm on all outside courts with the temperature around 35 degrees. Disappointed tennis fans huddled in groups at vendors selling hot drinks and food, and under whatever shelter they could find to wait out . Leaving everything behind, people are fleeing conflict in Ukraine. Headquarters in London, UK. This file contains bidirectional Unicode text that may be interpreted or compiled differently than what appears below. The flow characteristics over this barrier are similar to what Stull (1988) describes with respect to the down-slope wind storms associated with hydraulic jump. In addition to the qualitative overview of the vertical structure of the along-valley winds and potential temperature field, a more detailed analysis of how the depth of the daytime up-valley wind layer and the depth of the warmed layer relate to each other is now considered. Flows and Turbulent Convection in an Idealized Mountain Valley, J. (2015). Forecasts of Winter Precipitation Using an Improved Bulk Microphysics Scheme. These aims are addressed primarily by analysing a 4d simulation performed with the Weather Research and Forecasting (WRF) model, as the network of meteorological observations is rather scarce in this region. The default unit of measurement for wind speed is meter/second. (2021) analysed in their study. The valley atmospheres warm 46K between 09:00 and 15:00LT on20December. Similarly, the vertical extent of the amplified diurnal cycle of potential temperature is based on the model level at which the daily range in potential temperature is the same as over the plain (not shown, but three model levels are shown in Fig.11). Here i am accessing the weather data of Delhi city which is in India. There is a possibility to receive a central district of the city/town with its own parameters (geographic coordinates/id/name) in API response. Collier, E. and Immerzeel, W.W.: High-resolution modeling of atmospheric Meteorol. In this case, the API response should be returned in the same language as the language of requested location name if the location is in our predefined list of more than 200,000 locations. on Planetary Boundary Layer Growth Over a Valley on the North Side of the For both daytime and night-time, the RMSE in wind speed is lowest at Lukla and highest at NCO-P; moreover, the night-time RMSE is lower than the daytime value at each station. At Lukla, the amplitude of the daily cycle of temperature is not captured well (MAE of 2.3K), but the average temperature is closer to observations (daytime MBE of 0.5K and night-time MBE of 2.3K). Phys., 15, 65896603, https://doi.org/10.5194/acp-15-6589-2015, 2015.a, b, c, d, e, f, g, Whiteman, C. D.: Mountain Meteorology: Fundamentals and Applications, New York, Oxford University Press, Meteorol., 43, 170181. Bull. The valleys that we concentrate on have ridge-to-ridge distances of more than 30km (discussed in Sect.3). Up to 10ms1 wind speeds are simulated at the surface at higher elevations (i.e in the top parts of the Gaurishankar and Khumbu valleys; Fig.7a, b, c, d). One of the analysed locations, the middle of the top half of Kanchanjunga (red time series in Fig.7d), shows signs of a single circulation cell. Access current weather data for any location on Earth including over 200,000 The valley topographical characteristics are described in Sect.3. Such a single circulation cell spans the whole cross-valley direction and can be identified if there are daytime up-slope winds at one slope and down-slope winds at the other slope (Fig.S3h in the Supplement). Your Shopping Cart will be saved and you'll be given a link. G., Bidlot, J., Bonavita, M., DeChiara, G., Dahlgren, P., Dee, D., Geosci., 14, 49, Wind Speed %wind-speed% - Km/h for Metric, Mp/h for Imperial, Wind Direction %wind-dir% - Eg. (2010). The along-valley winds do not have a clear repetitive diurnal cycle at the valley top except on the last day of the simulation. 2018.a, b, c, Collier, E. and Immerzeel, W.W.: High-resolution modeling of atmospheric As a result I get a value which seems to be in m/s. diSarra, A.G., Evangelisti, F., Duchi, R., Facchini, M., Fuzzi, S., Gobbi, List of city ID 'city.list.json.gz' can be downloaded here. In the bottom right, click on the The threshold wind speed, below which reliable measurements cannot be obtained, for the anemometers measuring at all three stations is 0.21ms1 for wind speed and 0.15ms1 for wind direction. For each point on the globe, OpenWeather provides historical, current and forecasted weather data via light-speed APIs. At the valley entrance, the onset and peak in magnitude occur at the same time as in the other valleys, but the decay of the up-valley winds is slower; on 20 and 21December, the along-valley wind component only changes to the down-valley direction at around 02:0003:00LT. The cross-sections show the whole length of the valley centre lines (yellow lines in Fig.2b); thus, the far right-hand side of all the panels in Figs.8 and 9 are the wind component and potential temperature above the plain. Sci. OpenWeather is a team of IT experts and data scientists that has been practising deep weather data science. 2012 2022 OpenWeather All rights reserved, 8,000+ OpenWeatherMap weather API repositories on GitHub, Google Weather-Based Campaign Management with OpenWeatherMap API, Connect your weather station to OpenWeatherMap, Get weather data for free for open source project, Vegetation indicies statistics by each recognised field, Climate data for regions and particular field, Vegetation indices and Historical NDVI chart, Current, Forecast and Historical weather data. The along- and cross-valley wind characteristics in each of the four valleys are described in Sect.4. The yaxes are the grid points at the valley centre, and the crosses on the right-hand side of each figure denote the location of the grid points marked using the same colours in Figs.2b and 3. The up-valley wind propagation into the valley could be significantly interrupted by the flow forced to flow over the 1km high barrier. Adding OpenWeatherMap to your Home Assistant instance can be done via the user The up-valley winds basically stop on the northern side of the barrier close to the valley entrances of Gaurishankar and Khumbu. I would like to follow your blog frequently. Headquarters in London, UK. The scale measures multiple environmental factors: air temperature, radiant heat, humidity and wind speed, based on readings taken at five different locations around the tournament. I have used these in my own application to convert a JSON response of: 1 2 3 4 "wind": { "speed": 5.7, "deg": 50 }, into: Wind speed: 12.75 mph in a North East direction. The vertical extent of the amplified diurnal cycle of temperature seems to correlate with the up-valley wind layer depth in the valleys: where the amplified diurnal cycle of temperature reaches higher, the daytime up-valley winds also reach higher. Comparing the observed wind direction during the 1821December2014 study period (Bianchi etal.,2021) with other periods, such as the winters of 19941999 (Bollasina etal.,2002; Ueno and Kayastha,2001), December in 2003 (Ueno etal.,2008) and December in 2006 and 2007 (Bonasoni etal.,2010), the study period resembles the average wind conditions at the NCO-P station well. In the Gaurishankar and Khumbu valleys, the valley depth increases are not as gradual, but the valleys still get deeper from the valley entrance towards the valley top. During the 4d study period, the daytime up-valley winds are weaker and flow in a shallower layer in the parts of the valleys where the valley floor has a steep inclination (up to 5). The valleys are roughly northsouth orientated and are inclined towards the north, so the valleys face south. The up-valley wind layer is deepest in the portion of the Makalu (grid points 120160) and Kanchanjunga (grid points 70120) valleys with a flat valley floor, where the flow depth reach up to 1500m, and shallowest at the top of the Gaurishankar (grid points 2040) and Khumbu (grid points 3050) valleys, where the flow depth is less than 600m. Phys., 10, 75157531, https://doi.org/10.5194/acp-10-7515-2010, 2010.a, b, c, d, Bonekamp, P., Collier, E., and Immerzeel, W.: The Impact of Spatial Resolution, Figures10 and 11 show that the diurnal cycle of potential temperature reaches higher up in the valley atmosphere compared with over the plain. (2021) found that WRF struggled to accurately simulate the diurnal variation in wind speed, especially during daytime and when wind conditions changed from high to low, over the Central Himalayas. Here i have pretty printed the data, because JSON data is very difficult to read and thats why it should be pretty printed. ", Accessing Data For Cities Within A Rectangle Zone, "http://api.openweathermap.org/data/2.5/box/city? The simulation is evaluated using meteorological observations from three AWSs in the Khumbu Valley. LIVE UPDATES: Aussie world No. During night-time, the winds are around 2ms1 and are directed up-valley in the top half of the valley (grid points 25 and 45 in Fig.6a), and they are less than 1ms1 up- or down-valley in the lower half of the valley (grid points 70 and 95 in Fig.6a). So write the following code. You can insert the following DIV inside your documents to provide dynamic weather which is updated at the frequency set in the settings Update Frequency setting. The up-valley winds exceeding 3ms1 cover half of the along-valley distance in Kanchanjunga, whereas they are only found at the valley entrance in Makalu. We thank EmilyPotter and one anonymous referee for their comments which helped improve this paper. You can access data by passing city name or city name and country code. The tops of the Gaurishankar and Makalu valleys are favourable for large-scale north-westerlies to channel into the valley atmosphere. The number of missing time steps due to neglected wind speed measurements is two for Namche at night-time, three for Lukla during daytime and nine for Lukla at night-time. interface, by using this My button: If the above My button doesnt work, you can also perform the following steps The 40-year climatology considered is the average of the month of December in the period from 1980 to 2019. In Kanchanjunga Valley, the floor inclination ranges between 1 and 3 in the top half of the valley, between grid points 20 and 60. Where the valley floors start to incline strongly up towards the tops of the valleys is approximately where the warmed layer starts to become shallower. Due to computational and data storage limitations, it is not possible to perform a long-term simulation with high-temporal-resolution output. Sci. Clouds in the Himalayas: first two years of continuous observations at the The valley centre lines (in yellow in Fig.2b) were identified using a simple algorithm. The weather data is provided for any moment of time for 5 days ahead and 5 days back, covering any destination and any point along the route. A sensor entity will be created for each supported condition. The Weather Research and Forecasting model is run with a 1km horizontal grid spacing covering a 4d period in December2014. Sensors provide data in the language that was selected when configuring the integration. You might need to cast it to a QuantityType first. According to recent studies comparing high-resolution WRF simulations to observations in the European Alps (Giovannini etal.,2014a, b) and in the Himalayas (Collier and Immerzeel,2015; Karki etal.,2017; Potter etal.,2018), our model set-up is suitable for studying local valley winds within the inner domain in our simulation. Wang, W., Long, C., Chelliah, M., Xue, Y., Huang, B., Schemm, J.-K., The subtropical jet was located south-east of the inner domain (d04) location during the 1820December simulation period. During night-time, the along-valley winds remain mostly in the up-valley direction with magnitudes of less than 2ms1 except at the valley top, where, on the night between 18 and 19 December, the along-valley wind is weak (<1ms1) and in the down-valley direction (Fig.6). Now we will see how to access weather data in python using openweathermap API. Question 1: reanalysis, Q. J. Roy. We use the vector Ai=x(xi+3-xi-3)+y(yi+3-yi-3) to describe the local orientation of the valley at the ith grid point on the valley centre line. and Collins, W.D.: Radiative forcing by long-lived greenhouse gases: resolution on WRF v3.8.1 simulated meteorology over the central Himalaya, Red stars denote the location of Kathmandu (the furthest east star) and New Delhi. Dommen, J.: Biogenic particles formed in the Himalaya as an important source Learn how your comment data is processed. 7.7 * 3.6 = 27.7. The large-scale north-westerly winds at upper levels channel into the valleys, especially in the northernmost and thus highest parts of the Gaurishankar and Makalu valleys, on 18December and are seen as strong down-valley near-surface winds during the day (Fig.5a) and during the night between 17 and 18December (Fig.S2a and c in the Supplement). the Convection, Viscous Sublayer, and Turbulence Closure Schemes, Mon. Strong and shallow winds, resembling down-slope winds, are found on the leeward slope of the barrier followed by weaker and deeper winds at the valley entrance, 20km towards the valley from the barrier. So you can find the weather data by passing the longitude or latitude of a particular location. List of city ID 'city.list.json.gz' can be downloaded, For temperature in Fahrenheit use units=imperial, For temperature in Celsius use units=metric, Temperature in Kelvin is used by default, no need to use units parameter in API call. Wind speed: meter/sec : meter/sec : miles/hour : deg: Wind direction : degrees (meteorological) degrees (meteorological) degrees (meteorological) gust: . Meteorol., 43, 170181, Check weather updates with our OpenWeather feature that provides graphic overlays on the map for clouds, precipitation, sea level pressure, temperature, and wind speed. They found that the difference between 12h, 24h, and 3d spin-up time was relatively small (10m wind root-mean-square error of 3.5ms1 for 12h and of 3.3ms1 for 24h and 3d). Data is available in JSON, XML, or HTML format. Inness, P. and Dorling, S.: Operational Weather Forecasting,John Wiley&Sons,Ltd. Inoue, J.: Climate of Khumbu Himal, J. Jpn. The wind speed is mostly less than 2ms1 in the Gaurishankar and Khumbu valleys, and the flow depth above the valley centre line is 5001000m. If you need the geocoder to automatic convert city names and zip-codes to geo coordinates and the other way around, please use our, Your unique API key (you can always find it on your account page under the. Toggle display of the current weather in the statusbar on or off, Define your statusbar weather string here, Time interval to update the weather displayed in the statusbar and DIV's (1, 5, 10, 15, 20, 30 or 60 minutes). prediction, 1115, 2004.a, Thompson, G., Field, P.R., Rasmussen, R.M., and Hall, W.D.: Explicit As we focus on the along-valley winds, it is sensible to extend the valley centre lines towards the plain over this barrier instead of following the topography towards the south-east (Fig.2b). All authors discussed the final form of the manuscript. The amplitude of the diurnal cycle is slightly larger in the middle of the valley than at either the valley entrance or the valley top. 2010.a, Shea, J., Wagnon, P., Immerzeel, W., Biron, R., Brun, F., and Pellicciotti, F.: Positive values indicate higher potential temperatures at 15:00LT than at 09:00LT. You can use the lang parameter to get the output in your language. A variety of subscriptions with various limits on calls/min, data availability, and service. This is consistent with the stronger up-valley winds at this time in Kanchanjunga compared with the other valleys. Using only one API call, you can get Forecast (for 10 days with 3-hour step), Historical, and Current weather maps. If you dont pass country code thensearch works for USA as a default. Download OpenWeather and enjoy it on your iPhone, iPad and iPod touch. Home Assistant automatically translates it to the language configured for the frontend. simulations of boundary-layer processes and urban-induced alterations in an https://doi.org/10.1175/2010BAMS3001.1, 2010.a, Schmidli, J.: Daytime Heat Transfer Processes over Mountainous Terrain, J. Atmos. In the top of Gaurishankar Valley, the along-valley winds do not show a clear diurnal cycle except on the last day of the simulation. . Meteorol. Overall, the model manages to simulate the diurnal cycle of the winds that was evident in the observations. These weak down-valley winds are found in all of the valleys, but they only cover a minor share of the along-valley distance, and the up-valley winds are the dominant feature of the valley atmospheres, even in the morning. To make this data optional within your string you can surround it with the caret symbols. Learn more, City name. Sellegri, K., Yan, C., Worsnop, D., Kulmala, M., Baltensperger, U., and the Nepalese Himalaya, Int. The strongest warming between 09:00 and 15:00LT is found in the near-surface layer (i.e. geographic coordinates, zip/post code, city name, city ID, number of cities (only in current weather and forecast APIs). (2021) suggested that the daytime up-valley winds in the Khumbu Valley would transport aerosol precursors from the bottom of the valley to the free troposphere. Atmospheric pressure at sea level for the forecasts time period, hPa. The black star, blue cross, and red cross on the yellow line show the locations of the Nepal Climate Observatory Pyramid (NCO-P) station, the Namche AWS and the Lukla AWS respectively. Dynamical Drivers of the Local Wind Regime in a Himalayan Valley, J. Geophys. in formatted form. In Gaurishankar, the valley depth reaches around 2500m, whereas the valley depth in the other three valleys is larger (in the range of 35004000m). We support the following languages that you can use with the corresponded lang values: To use JavaScript code you can transfer callback functionName to JSONP callback. 25072522, https://doi.org/10.1175/2007MWR2298.1, 2008.a, b, c, Wagner, J. S., Gohm, A., and Rotach, M. W.: Influence of along-valley terrain heterogeneity on exchange processes over idealized valleys, Atmos. The easternmost valley, Kanchanjunga, is an exception here because it is surrounded by sufficiently high ridges on the sides and at the valley top (Fig.3d) that shelter the valley atmosphere from the large-scale flow channelling. Thank you @rlkoshak, the syntax for the rules was not fully correct but you put me on the right way. Daytime up-valley winds are found in all four valleys during the simulated 4d period. J. The along-valley wind component in Fig.6 is the average of five grid points along the valley centre line around the crosses to describe the wind in a larger part of the valley, instead of only at one grid point. For each point on the globe, OpenWeather provides historical, current and forecasted weather data via light-speed APIs. The simulation was kept on track by nudging the temperature, horizontal wind components and specific humidity in the outer domain (d01) towards the reanalysis every 6h. The contact author has declared that none of the authors has any competing interests. For each point on the globe, OpenWeather provides historical, current and . high altitude in the Khumbu Valley, Nepal Himalayas, 19941999, Bull. MB contributed to the understanding and interpretation of the simulation results, particularly in terms of the mesoscale dynamics. OpenWeather Dashboard is a visual tool for working with weather data and timely tracking of dangerous phenomena. Makalu and Kanchanjunga have rather flat valley floors from the valley entrance into the valley, with less than a 1 inclination (brown shading in Fig.3c and d). G.P., Maione, M., Panday, A., Roccato, F., Sellegri, K., Venzac, H., Verza, Id prefer to get in km/h but I cannot find any way of doing that. to retrieve the five day weather forecast by the geographical coordinates you specify. Saha, S., Moorthi, S., Pan, H.-L., Wu, X., Wang, J., Nadiga, S., Tripp, P., In the afternoon, all of the valley atmospheres are 35K warmer in middle of the valley (purple crosses) compared with the same altitude above the plain (Fig.9). Rotach, M.W., Wohlfahrt, G., Hansel, A., Reif, M., Wagner, J., and Gohm, A.: Keep Rocking!! For each point on the globe, OpenWeather provides historical . # JSON data works just similar to python dictionary and you can access the value using []. - Sixth line is the wind speed in m/s. I found a very similar issue in OH1 : Although the large-scale flow during the studied 4d period is similar to the 40-year climatology, the results are subject to uncertainty, due to the short simulation period, and may not be valid under different or more time-variable large-scale forcing. However, the timing of the diurnal cycle is well captured at all three stations (Fig.S1b, d and f in the Supplement). Temperature is available in Fahrenheit, Celsius and Kelvin units.